{"title":"Books","description":"","products":[{"product_id":"972","title":"Records of the Geological Survey of New South Wales: Volume 23, Part 1","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThis report covers the area between Forbes in the south, and Tomingley in the north, and the Harvey Range and Carridgery-Gunning Ridge in the east and west respectively.\u003c\/p\u003e\n\u003cp\u003eA meridional belt of gold deposits extending from Forbes, through Parkes and Peak Hill to Tomingley and a significant new discovery of a porphyry copper-gold province near Goonumbla, have recently provided the stimulus for a high level of exploration activity in the area. \u003c\/p\u003e\n\u003cp\u003eSeveral sub-projects of the Geological Survey's Component of the Parkes Project are discussed in this report.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cspan\u003eRecord 23 1990. Department of Mineral Resources and Development, Geological Survey of New South Wales.\u003c\/span\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eComments\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cspan\u003ePublication is now out of print. \u003c\/span\u003e\u003cspan\u003eDigital copies of the book can now be found and downloaded on DIGS.\u003cbr\u003e\u003c\/span\u003e\u003ca href=\"https:\/\/search.geoscience.nsw.gov.au\/product\/943\" rel=\"noopener\" target=\"_blank\"\u003e\u003cspan\u003ehttps:\/\/search.geoscience.nsw.gov.au\/product\/943\u003c\/span\u003e\u003c\/a\u003e\u003cbr\u003e\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744749523102,"sku":"DRNSW_MEG_GSNSW_972","price":38.5,"currency_code":"AUD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_943.jpg?v=1593054340"},{"product_id":"973","title":"Permian Foraminifera of the Sydney Basin, Memoir Palaeontology No. 19, 1982","description":"\u003ch4\u003eAbstract\u003c\/h4\u003e\n\u003cp\u003eMost of the Permian sequence of the Sydney Basin is of marine origin, and Foraminifera occur throughout the Permian section, including marine intercalations in the uppermost part of the section known for economically important coal deposits. Permian foraminiferal faunas of the Sydney Basin (and of Australia) are characterised by the following features;\u003c\/p\u003e\n\u003cul\u003e\n\u003cli\u003eabsence of fusulinid foraminifera and conodonts;\u003c\/li\u003e\n\u003cli\u003eabundance of agglutinated forms;\u003c\/li\u003e\n\u003cli\u003eintermittent occurrence of calcareous Nodosariidae and Miliolacea;\u003c\/li\u003e\n\u003cli\u003esouth-north differentiation of foraminiferal faunas; and\u003c\/li\u003e\n\u003cli\u003esome east-west differentiation, since some genera known to occur in Western Australia have not been found in the Sydney Basin.\u003c\/li\u003e\n\u003c\/ul\u003e\n\u003cp\u003eIt is quite clear from the palaeogeography of the Permian that the northern lithostratigraphic units were further away from the Permian shoreline than their southern equivalents and so a less turbulent environment can be expected for them.\u003c\/p\u003e\n\u003ch4\u003eReference\u003c\/h4\u003e\n\u003cp\u003eScheibnerova V. 1982. Permian Foraminifera of the Sydney Basin. Geological Survey of New South Wales, Memoir Palaeontology 19, 136 pp.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eComments\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cspan\u003ePublication is now out of print. \u003c\/span\u003e\u003cspan\u003eDigital copies of the book can now be found and downloaded on DIGS.\u003cbr\u003e\u003c\/span\u003e\u003ca href=\"https:\/\/search.geoscience.nsw.gov.au\/product\/947\" target=\"_blank\" rel=\"noopener\"\u003e\u003cspan\u003ehttps:\/\/search.geoscience.nsw.gov.au\/product\/947\u003c\/span\u003e\u003c\/a\u003e\u003cbr\u003e\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744749555870,"sku":"DRNSW_MEG_GSNSW_973","price":11.55,"currency_code":"AUD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/palaeomemoir19.jpg?v=1776390322"},{"product_id":"746","title":"Torrowangee-Fowlers Gap Explanatory Notes, 1:100,000, 1978","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Fowlers Gap and Torrowangee 1:100,000 sheets lie to the north of Broken Hill. The two map sheets cover and area of approximately 5200 km2. The aim of this work was primarily the elucidation of the Adelaidean stratigraphy and correlation with similar sequences on South Australia. Information on the Willyama Complex and Late Devonian sediments is mostly from existing thesis work.\u003c\/p\u003e\n\u003cp\u003eThe area covered by this study is mainly part of the Adelaide Fold Belt: a minor area in the northeast belongs to the Kanmantoo Fold Belt (Scheibner 1974). The Adelaide Fold Belt consists of several. Old, uplifted, fault-bounded anticlinorial blocks which are aspirated by synclinorial zones of relatively unmetamorphosed sediments.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eCooper P.F., Tuckwell K.D., Gilligan L.B. and Meares R.M.D., 1978. Geolology of the Torrowangee and Fowlers Gap 1:100,000 Sheets 7135, 7235. Geological Survey of New South Wales, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744750145694,"sku":"DRNSW_MEG_GSNSW_746","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/torrowangeeexplannotes.jpg?v=1777338077"},{"product_id":"747","title":"Tumut 1:100,000 Explanatory Notes, 1990","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Tumut 1:100,000 map sheet area (part of the Wagga Wagga 1:250,000 map sheet area) covers part of the southwestern slopes region. The rocks are in (from west to east) the Wagga Anticlinorial Zone, Tumut Synclinorial Zone and Young Anticlinorial Zone of the Lachlan Fold Belt. Oldest rocks are the ?Cambrian-Early Ordovician Jindalee Group, a sequence of metamorphosed sedimentary and igneous rocks (including the Gundagai Serpentinite). Middle Ordovician to Early Silurian rocks include sedimentary rocks of the Wagga Metamorphic Belt, the Nacka Nacka Metabasic Igneous Complex - and dioritic to granodioritic intrusions.\u003c\/p\u003e\n\u003cp\u003eDuring the Early to Late Silurian a complex sequence of igneous and sedimentary rocks were deposited or emplaced - including the Coolac Serpentinite, the Honeysuckle Metabasic Igneous Complex, Jackalass Slate, Blowering Formation, Goobarragandra Volcanics and the Young Granodiorite. Some of these units are extensive - in thickness and areal extent. Early Devonian volcanic units and granites (such as the Bogong Granite) were the last of the Palaeozoic rocks formed in the Tumut 1:100,000 map sheet area. The geological history discussed in the Notes is from the perspective of terrane analysis. Younger units include a Jurassic lamprophyre dyke and Cainozoic igneous and sedimentary units - including sands and gravels (with some high-level sediments worked for gold.\u003c\/p\u003e\n\u003cp\u003eMost of the 295 metallic mineral deposits shown on the map contain gold. Hard-rock gold occurrences are widespread: veins (in various units); reefs in the Nack Nacka Metabasic Igneous Complex; and veins and fissure fillings in a wide range of rocks. Many of the gold occurrences were found in the Adelong Creek Goldfield - and there are four other declared goldfields. Most of the (hard-rock) gold occurrences seem to be of metamorphic hydrothermal origin. Other metallic mineral deposits include copper (and lead and zinc), chromium, tin, molybdenum, manganese and iron.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eBasden H., 1990. Geology of Tumut 1:100,000 Sheet 8527. 275 pp. New South Wales Geological Survey, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744751751326,"sku":"DRNSW_MEG_GSNSW_747","price":22.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/tumutexplantory.jpg?v=1777343441"},{"product_id":"748","title":"Wollongong-Port Hacking Explanatory Notes, 1:100,000, 1986","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Wollongong-Port hacking 1:100,000 Geological Sheet covers much of the southern part of the Sydney Basin. Rocks of Permian and Triassic age crop out with similar areas of Cainozoic sediments, and volcanic rocks ranging in age from Jurassic to late Tertiary.\u003c\/p\u003e\n\u003cp\u003eThis area contains widespread economic deposits of Permian coal and lies within the Southern Coalfield. Coal was first recorded in 1796 by Bass and Flinders and mined as early as 1828.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eSherwin L., and Holmes G.G., (Eds), 1986. Geology of the Wollongong and Port Hacking 1:100,000 Sheets 9029, 9129. 179 pp. New South Wales Geological Survey, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744754176158,"sku":"DRNSW_MEG_GSNSW_748","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/wollongongporthacknotes.jpg?v=1777526635"},{"product_id":"256","title":"Ana Branch Explanatory Notes, 1:250,000, 1996","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe 1:250,000 map sheet area is located in the south-west corner of New South Wales with low relief and consists of sandplains and dunefields. The map area is located entirely within the Murray Basin, a shallow intercratonic basin underlain by the Kanmantoo Fold Belt. The rocks underlying the sediments and sedimentary rocks of the Murray Basin fall within two structural belts, the Glenelg Zone and the Morden-Stawell Zone.\u003c\/p\u003e\n\u003cp\u003eThe oldest rocks are the Late Proterozoic to Cambrian sedimentary and mafic igneous rocks of the Kars Block. Cretaceous sandstone units are more widespread and covers almost the whole map area. Overlying all earlier units are poorly lithified to unconsolidated sediments of the Tertiary Murray Basin sequences. A few outcrops of lacustrine sediments of Late Pliocene to Pleistocene age and aeolian sands have been found. \u003c\/p\u003e\n\u003cp\u003eExploration for heavy mineral sand deposits have been active in the Murray Basin area resulting in the discovery of the Mt Massidon deposit in the Pleistocene Loxton-Parilla sands. The Tararra and Wentworth Infrabasins are considered to have potential for the discovery of petroleum and possibly coal seam methane. Geological and geomorphological features were obtained from aerial photographs, interpretation of lineaments and palaeogeographic features were carried out with the aid of Landsat and NOAA imagery.\u003c\/p\u003e\n\u003cp\u003eField checking and sampling were also carried out and the information were digitised on the Mineral Resource Land Information System.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eRay H.N. (Facer R.A. ed.) 1996. Ana Branch 1:250,000 Geological Sheet SI\/54-7: Explanatory Notes. Geological Survey of New South Wales, Sydney, viii+96pp.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744754569374,"sku":"DRNSW_MEG_GSNSW_256","price":33.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/anabranchbook.jpg?v=1773095298"},{"product_id":"561","title":"Booligal Explanatory Notes, 1:250,000, 1997","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Booligal 1:250,000 map sheet area is flat, semi-arid and dominated by interacting Quaternary morphostratigraphic units. The study area is almost entirely covered with unconsolidated and consolidated sediments of the Murray Basin, and the basement consists for the great part of Lachlan Fold Belt rocks.\u003c\/p\u003e\n\u003cp\u003eThe study area lies within the eastern part of the Murray Basin and consists of fluvial and possible marginal Tertiary sedimentary units deposited in an interactive setting. Sedimentary thickness vary from 20m to 200m overlying basement highs and from 200m to 410m within basement troughs.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eCameron R.G., 1997. Booligal 1:250 000 Geological Sheet SI\/55-5: Explanatory Notes. Geological Survey of New South Wales, Sydney, x + 94 pp.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744759681182,"sku":"DRNSW_MEG_GSNSW_561","price":33.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_450.jpg?v=1593054371"},{"product_id":"564","title":"Cootamundra Explanatory Notes, 1:250,000, 1995","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThese notes and the accompanying map contain descriptions of the geological units that occur on the Cootamundra 1:250,000 map sheet area, as well as information on the geological history, structural geology, mineral deposits and regional geophysics of the area. Descriptions in the Mineral Deposit section only provide information on selected occurrences, particularly the gold deposits of West Wyalong-Temora-Adelong belt. Only minor changes have been made to earlier geological mapping on the eastern part of the map sheet area.\u003c\/p\u003e\n\u003cp\u003eWork has concentrated on the central and western parts and has indicated that late Ordovician to early Silurian intermediate to basic volcanic rocks and their intrusive equivalents are widespread. A four-fold subdivision has been based on major fault structures. These four zones are: the Western or Wagga Zone; the Western Central Zone; the Eastern Central Zone; and the Young Zone. Deformation in the late Silurian led to closure of the Tumut Trough with possible obduction of the Coolac Serpentinite and the North Mooney Complex to their present positions. Age determinations, palaeontological data, selected geochemical data and list of mineral deposits are included.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eWarren A.Y.E., Gilligan L.B. and Raphael N.M. 1995. Geology of the Cootamundra 1:250,000 map Sheet. viii + 160 pp. Geological Survey of New South Wales, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744763973790,"sku":"DRNSW_MEG_GSNSW_564","price":33.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_452.jpg?v=1593054376"},{"product_id":"566","title":"Narromine Explanatory Notes, 1:250,000, 1996","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe area covers the Narromine 1:250,000 map sheet, with mostly very low relief and is more than half covered by surficial deposits. Most rock units are deeply weathered and good exposures are generally limited to quarries, road and railway cuttings.\u003c\/p\u003e\n\u003cp\u003eThe area is of significant economic importance as it contains the North Parkes copper and gold mine as well as other gold, base metal and platinum group metals occurrences. The western third of the area has the multiply deformed Girilamborne Group, consisting mostly of quartzite, phyllite and schist as basement.\u003c\/p\u003e\n\u003cp\u003eThe eastern two thirds of the map area comprises the Early Ordovician Nelungaloo Volcanics and Late Ordovician trachyandesitic Goonumbla Volcanics and silicious sediments of the Cotton Formation. Granites are predominantly of the I type, intruded in the Early to Late Devonian. Canozoic volcanism is restricted to the north east, while alluvial plains have an ill defined basal Tertiary age and extent into the Recent.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eSherwin I., 1996. Narromine 1 :250,000 Geological Sheet SI\/55-3: Explanatory Notes, viii + 104 pp. Geological Survey of New South Wales, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744767053982,"sku":"DRNSW_MEG_GSNSW_566","price":33.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/narrominenotes.jpg?v=1776227604"},{"product_id":"567","title":"Nyngan and Walgett Explanatory Notes, 1:250,000, 1996","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eLocated in the northern part of Lachlan Fold Belt, in semi-arid north-western New South Wales, the Nyngan and Walgett 1:250,000 map sheet areas consist largely of flat to gently sloping alluvial plains. Quaternary alluvium up to 100m thick covers 90% of the area.\u003c\/p\u003e\n\u003cp\u003eFive major meridional structural zones of buried Palaeozoic basement were interpreted from geophysical data and water bore logs. Basement youngs from Cambro-Ordovician in the west to Siluro-Devonian in the east. The overlying Jurassic to Cretaceous sequence of the Great Australian Basin represents a period of terrestrial to marine deposition.\u003c\/p\u003e\n\u003cp\u003eMajor Cainozoic depocentres are located in the central northern Walgett sheet area and in the north-east of the Nyngan sheet area. Several sources of loam, sand, gravel and aggregate are exploited in the area. There is also potential for copper and platinum group metals (PGM) mineralisation in the Girilambone Structural Zone, porphyry style copper-gold in the Parkes Structural Zone, and opal within the Cretaceous sequence.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eWatkins J.K. and Meakin N.S. 1996. Nyngan and Walgett 1:250,000 Geological Sheets SH\/55-15 \u0026amp; SH\/55-11: Explanatory Notes, viii + 112 pp. Geological Survey of New South Wales, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744768561310,"sku":"DRNSW_MEG_GSNSW_567","price":33.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_455.jpg?v=1593054388"},{"product_id":"568","title":"Pooncarie Explanatory Notes, 1:250,000, 1996","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe area lies within the eastern part of the Murray Basin. Most of that area consists of fluvial and marine Tertiary sedimentary units deposited in an intracratonic setting. Sediment thickness varies from 80m to 150m overlying basement highs and from 280m to 320m within basement troughs. Outcropping basement rocks occur in two parts of the area: Manfred Range and 'Springhill' property. The buried pre-Tertiary surface consists of a series of elongated ridges and valleys.\u003c\/p\u003e\n\u003cp\u003eThe major palaeo-physiographic features, some of which are structural, have been identified. There are two aquifier-bearing depositionl sequences within the Tertiary succession. At least four forms of capping silcrete are present. They formed on outcropping Plio-Pleistocene clay-cemented quartz arenites, primarily the Parilla Sand, probably around 0.7 Ma to 0.4 Ma ago. Nearby Pliocence-hosted heavy mineral sands deposits are potential sources of titania for the silcretes.\u003c\/p\u003e\n\u003cp\u003eThe extensive, flat, semi-arid Pooncarie map area is areally dominated by interacting Quaternary morphostratigraphic units of aeolian, lacustrine and fluvial depositional systems that are now largely inactive. Pliocene marine Loxton Sands - hosted heavy mineral sand deposits were formed as beach placers in topographic embayments. These deposits are presently considered sub-economic.\u003c\/p\u003e\n\u003cp\u003eOther mineral deposits, albeit also of limited economic potential, include gypsum and oolitic iron deposits, and lignite. A bentonite deposit, however, at Arumpo has considerable potential.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eCameron R.G. (Facer R.A. ed.) 1996. Geology of Pooncarie 1:250,000 map. Geological Survey of New South Wales, Sydney, xii + 108 pp.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744770035870,"sku":"DRNSW_MEG_GSNSW_568","price":33.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/pooncarienotes.jpg?v=1776400234"},{"product_id":"1597","title":"Cobar 1:250,000 Metallogenic Map: Metallogenic Study and Mineral Deposit Data Sheets, 1994","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eTwo hundred and sixty two mineral occurrences are documented in the data sheet and plotted on the accompanying Cobar 1:250,000 Metallogenic Map. These notes are based on an extensive compilation of the mineral occurrences in the area undertaken in the mid to late 1970s.\u003c\/p\u003e\n\u003cp\u003eThis publication presents the most recent results on the geology and tectonic studies of Cobar area. Mineralisation styles are examined with some detailed descriptions of major deposits in the area. Details are given for each individual mineral occurrence \/ deposit in the data sheet, including mine name, location, mining history, host, deposit character, remarks and references.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eGilligan L.B. and Byrnes J.G., 1994. Cobar 1:250,000 Metallogenic Map SH\/55-14: Metallogenic Study and Mineral Deposit Data Sheets. 240 pp. Geological Survey of New South Wales, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744771281054,"sku":"DRNSW_MEG_GSNSW_1597","price":22.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/cobarmetnotes.jpg?v=1773632932"},{"product_id":"1599","title":"Dubbo 1:250,000 Metallogenic Map: Metallogenic Study and Mineral Deposit Data Sheets, 1975","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eAs part of the mapping project, as detailed a summary as possible was compiled for each mine. These summaries are presented in the form of data sheets. Much of the information contained on the data sheets is depicted in symbol form on the map in order to show regional settings more clearly and to give an overall picture of metallogenic provinces and\/or districts. It is hoped that the metallogenic maps and data sheets will be used as exploration tools.\u003c\/p\u003e\n\u003cp\u003eAs far as possible, no interpretation has been carried out in the assembly of this summary information so that independent workers may carry out their own analyses. The genetic discussion is purely interpretative, and is based on as much information as the writer has been able to gather on possible ore genesis, similarities and differences of deposits, and metallogenic districts or provinces. As a result some of the comments made in this section are quite conjectural.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eMatson C.R. 1975., Part 1 Mine Data Sheets to accompany Metallogenic Map Dubbo 1:250000. Part 2 Metallogenic Study of the Dubbo 1:250,000 Sheet. Geological Survey of New South Wales. 352 pp.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744772821150,"sku":"DRNSW_MEG_GSNSW_1599","price":22.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/dubbometnotes.jpg?v=1773970010"},{"product_id":"1603","title":"Grafton-Maclean 1:250,000 Metallogenic Map: Metallogenic Study and Mineral Deposit Data Sheets, 2001","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Grafton-Maclean 1:250,000 map sheet area is the most mineralised map sheet area in the New England region with a wide range of commodity and deposit types.\u003c\/p\u003e\n\u003cp\u003eMajor commodities include tin, tungsten, molybdenum, gold, arsenic, chromium, asbestos and topaz. Types of mineralisation present in the area include:\u003c\/p\u003e\n\u003cul\u003e\n\u003cli\u003ehydrothermal granite-related pipes, veins, multiveins, sheeted veins, stockworks, greisens and disseminations;\u003c\/li\u003e\n\u003cli\u003emetahydrothermal gold, antimony and mercury;\u003c\/li\u003e\n\u003cli\u003eophiolite-related chromium and asbestos;\u003c\/li\u003e\n\u003cli\u003eskarn occurrences; and\u003c\/li\u003e\n\u003cli\u003ealluvial, eluvial and deep lead tin, alluvial gold and sapphires and heavy mineral sands. \u003c\/li\u003e\n\u003c\/ul\u003e\n\u003cp\u003eThis metallogenic study forms the basis for renewed minerals exploration in the region. Mineralisation associated with granites, especially leucocratic granites, is a particularly attractive exploration target. Data collected during this study indicate that there is a particularly high potential for polymetallic mineralisation associated with buried granitoid bodies. High-resolution geophysics, together with the data presented in these Notes, would indicate areas amenable for further intensive exploration.\u003c\/p\u003e\n\u003cp\u003eMineralisation offering the greatest exploration potential includes:\u003c\/p\u003e\n\u003cul\u003e\n\u003cli\u003edisseminated gold associated with Early Triassic leucogranites;\u003c\/li\u003e\n\u003cli\u003emetahydrothemal gold;\u003c\/li\u003e\n\u003cli\u003ealluvial and deep lead tin in the Emmaville'Mole Granite area;\u003c\/li\u003e\n\u003cli\u003elarge-tonnage\/low-grade hard-rock tin (Taronga type);\u003c\/li\u003e\n\u003cli\u003elarge-tonnage\/low-grade deposits of tin, tungsten, molybdenum (Glen Eden type);\u003c\/li\u003e\n\u003cli\u003ebase metals associated with granitoids (Cangai copper type);\u003c\/li\u003e\n\u003cli\u003ebase metals associated with the Drake Volcanics;\u003c\/li\u003e\n\u003cli\u003eemeralds associated with the Mole Granite; - silexite;\u003c\/li\u003e\n\u003cli\u003ealluvial sapphire; and\u003c\/li\u003e\n\u003cli\u003egas and petroleum associated with the Clarence-Moreton Basin and related rocks.\u003c\/li\u003e\n\u003c\/ul\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eHenley H.F., Brown R.E., Brownlow J.W., Barnes R.G., Stroud W.J., \u0026amp; Facer R. (ed). 2001. 1:250,000 Grafton Maclean Metallogenic Map. Metallogenic Study and Mineral Deposit Data Sheets. Geological Survey of New South Wales.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744774492318,"sku":"DRNSW_MEG_GSNSW_1603","price":49.5,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/graftonmacleanmetnotes.jpg?v=1774481640"},{"product_id":"1605","title":"Inverell 1:250,000 Metallogenic Map: Metallogenic Study and Mineral Deposit Data Sheets, 1997","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eInverell map sheet 1:250,000 is one of the most extensively mineralised regions in the New England area. Significant mineral commodities include cassiterite, gold, base-metals, wolframite, diamonds and sapphires with minor deposits of fluorite, bauxite, clays, manganese oxide\/rhodonite, chromite, limestone.\u003c\/p\u003e\n\u003cp\u003eThe report presents results of the Inverell 1:250,000 scale Metallogenic mapping involving the assessment of the mineral resources of the New England Fold Belt in New South Wales. The results are presented in three parts:\u003c\/p\u003e\n\u003cul\u003e\n\u003cli\u003eMetallogenic Map, displaying all recorded mineral occurrences in the context of the revised geological framework,\u003c\/li\u003e\n\u003cli\u003eMetallogenic Study, including a summary of the regional geological setting and a description of the deposit types and finally\u003c\/li\u003e\n\u003cli\u003eMineral Deposit Data Sheets, including explanatory notes, a comprehensive deposit index and lists of unpublished reports and other references used in compiling the data sheets.\u003c\/li\u003e\n\u003c\/ul\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eBrown, R.E. \u0026amp; Stroud, W.J. 1997. Inverell 1:250,000 Metallogenic Map SH\/56-5: Metallogenic Study and Mineral Deposit Data Sheets. Geological Survey of New South Wales, Sydney, viii +576 pp. Edited by J.R. Stewart.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744775573662,"sku":"DRNSW_MEG_GSNSW_1605","price":33.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/inverellmetnotes.jpg?v=1774838302"},{"product_id":"1606","title":"Manilla-Narrabri 1:250,000 Metallogenic Map: Metallogenic Study and Mineral Deposit Data Sheets, 1992","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThis publication provides a comprehensive mineral deposit data base for the region, a modern recompilation of the geological data, and a regional metallogenic framework for use in mineral exploration, land - use planning and mineral resource management.\u003c\/p\u003e\n\u003cp\u003eThe information are presented in three parts:\u003c\/p\u003e\n\u003cul\u003e\n\u003cli\u003eMetallogenic map,\u003c\/li\u003e\n\u003cli\u003eMetallogenic study and\u003c\/li\u003e\n\u003cli\u003eMineral deposit data sheets.\u003c\/li\u003e\n\u003c\/ul\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eBrown R.E., Brownlow J.W. \u0026amp; Krynen J.P. 1992. Manilla-Narrabri 1:250,000 Metallogenic Map SH\/56-9, SH\/55-12: Metallogenic Study and Mineral Deposit Data Sheets. 319 pp. Geological Survey of New South Wales, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744776687774,"sku":"DRNSW_MEG_GSNSW_1606","price":22.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/manillanarrabrimetnotes.jpg?v=1775085814"},{"product_id":"1607","title":"Narromine 1:250,000 Metallogenic Map: Mine Data Sheets and Metallogenic Study, 1979","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe metallogenic study of the Narromine 1:250,000 sheet area is part of and concludes a major project aimed at providing an inventory of mineral deposits and an understanding of the metallogenesis of individual 1:250,000 sheet areas in the eastern Lachlan Fold Belt.\u003c\/p\u003e\n\u003cp\u003eThe geology and tectonics are briefly discussed in order to provide a framework for the discussion of the metallogensis. A discussion of the basis on which the deposits are classified and described follows the section on geology.\u003c\/p\u003e\n\u003cp\u003eThe text concludes with some thoughts on the direction future exploration sheet area should take.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eBowman H.N., Richardson S.J., \u0026amp; Dolanski J. 1979. Narromine 1:250,000 Metallogenic Map SI5503 Mine Data Sheets and Metallogenic Study. Geological Survey of New South Wales. 331 pp.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744778031262,"sku":"DRNSW_MEG_GSNSW_1607","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/narrominemetnotes.jpg?v=1776227866"},{"product_id":"1609","title":"Nymagee 1:250,000 Metallogenic Map: Metallogenic Study and Mineral Deposit Data Sheets, 1993","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Nymagee 1:250,000 Metallogenic map (SI5502) is produced as a part of a programme involving the assessment of the mineral resources of the Lachlan Fold Belt in New South Wales. This Metallogenic map and accompanying mineral deposit data sheets provide a comprehensive mineral deposit data base for the region, a modern recompilation of the geological data, and a regional metallogenic framework for use in mineral exploration, land use planning, mineral resource assessment.\u003c\/p\u003e\n\u003cp\u003eThe results of the Metallogenic Mapping Programme are presented in two parts:\u003c\/p\u003e\n\u003cul\u003e\n\u003cli\u003eMetallogenic Map,\u003c\/li\u003e\n\u003cli\u003eMineral Deposit Data Sheets, including explanatory notes, a comprehensive deposit index, and the lists of unpublished reports and other author-indicated references used in compiling the data sheets and finally\u003c\/li\u003e\n\u003cli\u003eMetallogenic Study, including a summary of the regional geological setting and a brief description of the deposit types.\u003c\/li\u003e\n\u003c\/ul\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eSuppel D.W. and Gilligan L.B. 1993. Nymagee 1:250,000 Metallogenic Map S1\/55-2:  Metallogenic Study and Mineral Deposit Data Sheets. 171 pp. Geological Survey of New South Wales, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744779899038,"sku":"DRNSW_MEG_GSNSW_1609","price":22.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/nymagee250metnotes.jpg?v=1776315417"},{"product_id":"768","title":"Metallogenic studies of the Broken Hill and Euriowie Blocks, New South Wales, Mineral Deposits of the Northern Broken Hill Block, 2003, Bulletin No. 32(5)","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Broken Hill Block in western New South Wales is host to one of the world's great lead-zinc-silver deposits. This report is the fifth in a series of descriptions of the metallogenesis of the Broken Hill and adjacent Euriowie Blocks. The Broken Hill Block North 1:50,000 metallogenic map area contains a wide variety of mineral deposit types, and many significant prospects. Nearly all of the 1,300 mineral occurrences shown on the map are hosted by the Early Proterozoic Willyama Supergroup, a metasedimentary sequence, with lesser metamorphosed acid and basic magmatic rocks.\u003c\/p\u003e\n\u003cp\u003eThe northern part of the Broken Hill Block includes the areas of lowest metamorphic grade, permitting a better understanding of the geology, rock types and some mineral deposit types. Stratiform deposits include Broken Hill type, Ettlewood type, Corruga type, Sisters type, and Great Eastern type deposits. Broken Hill type deposits consist of lead-zinc sulphide concentrations with associated granular quartz-gahnite\/garnet \"lode horizons\". They occur in clusters, with small, but significant production from the Allendale and Southern Cross-Parnell mines. Drilling at the Stephens Trig and Peppertree prospects obtained some of the best lead-zinc intersections found outside the Broken Hill Main Lode.\u003c\/p\u003e\n\u003cp\u003eEttlewood type deposits are confined to the Ettlewood Calc-Silicate Member. This type contains significant amounts of scheelite, sphalerite and minor galena, but the known calc-silicate bodies are too small to host an orebody. Corruga type deposits are hosted by Broken Hill Group calc-silicate rocks with an irregular texture, and contain base metal sulphides and\/or scheelite. In the Broken Hill Block North area, they have shown limited prospectivity, but may help delineate Broken Hill type ore-forming systems.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eStevens B.P.J., Barnes RG., Raphael N.M. \u0026amp; Burton G.R 2003. Metallogenic studies of the Broken Hill and Euriowie Blocks, New South Wales. 5. Mineral deposits of the northern Broken Hill Block. Geological Survey of New South Wales, Bulletin 32(5), xii + 244 pp.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744781373598,"sku":"DRNSW_MEG_GSNSW_768","price":66.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/bulletin32_5.jpg?v=1773356378"},{"product_id":"769","title":"Metallogenic Studies of the Broken Hill and Euriowie Blocks, New South Wales, Mineral Deposits of the Southern Eastern Broken Hill Block, 1993, Bulletin No. 32(4)","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThis study constitutes Part 4 of Bulletin 32 'Metallogenic Studies of the Broken Hill and Euriowie Blocks, New South Wales'. Although this report deals with the mineral occurrences within the Euriowie Block, those occurrences at the extreme northern end of the Broken Hill Block and in the Poolamacca Inlier are also discussed.\u003c\/p\u003e\n\u003cp\u003eThe blocks comprise rocks of the Palaeoproterozoic Willyama Supergroup which are considered to have been deposited within an intracratonic rift environment. They have regional metamorphism grading from greenschist to granitic facies, and later retrograde metamorphism. It covers the main Pb-Zn-Ag lodes and describes the lode geometry, mineralogy, host rocks, stratigraphy, structural setting and historical information on production and exploration.\u003c\/p\u003e\n\u003cp\u003eThe most important mineral deposits in this area are:\u003c\/p\u003e\n\u003cul\u003e\n\u003cli\u003estratiform type deposits,\u003c\/li\u003e\n\u003cli\u003ebase metal-bearing and gold-bearing vein deposits,\u003c\/li\u003e\n\u003cli\u003emineralisation related to intrusive rocks and non-metallic deposits.\u003c\/li\u003e\n\u003c\/ul\u003e\n\u003cp\u003eThe stratiform deposits are the most common and they are described in great detail. The text is well illustrated with figures and photographs. Interpreted geology with cross sections of several mines are presented. Summary of geochemistry assays of samples from three mines are presented in tables.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eBurton G.R. 2000. Metallogenic studies of the Broken Hill and Euriowie Blocks, New South Wales. 4. Mineral deposits of the Euriowie Block (including the northernmost Broken Hill Block and Poolamacca Inlier). Geological Survey of New South Wales , Bulletin 32(4), vi + 106 pp.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744781471902,"sku":"DRNSW_MEG_GSNSW_769","price":38.5,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/bulletin32_4.jpg?v=1773356237"},{"product_id":"770","title":"Metallogenic Studies of the Broken Hill and Euriowie Blocks, New South Wales, Mineral Deposits of the South Eastern Broken Hill Block, Bulletin No. 32(3)","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThis study of the mineral deposits of the south-eastern part of the Broken Hill Block is the third part of Bulletin No. 32 - Metallogenic Studies of the Broken Hill and Euriowie Blocks, New South Wales. It covers the main Pb-Zn-Ag lodes and describes the lode geometry, mineralogy, host rocks, stratigraphy, structural setting and historical information on production and exploration.\u003c\/p\u003e\n\u003cp\u003eThe most important mineral deposits in this area are:\u003c\/p\u003e\n\u003cul\u003e\n\u003cli\u003estratiform type deposits,\u003c\/li\u003e\n\u003cli\u003ebase metal-bearing and gold-bearing vein deposits,\u003c\/li\u003e\n\u003cli\u003emineralisation related to intrusive rocks and non-metallic deposits.\u003c\/li\u003e\n\u003c\/ul\u003e\n\u003cp\u003eThe stratiform deposits are the most common and they are described in great detail. The text is well illustrated with 41 figures and 17 photographs. Interpreted geology with cross sections of several mines are presented. Summary of geochemistry assays of samples from three mines are presented in tables.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eBurton G.R. 1994. Metallogenic studies of the Broken Hill and Euriowie Blocks, New South Wales. 3.Mineral deposits of the South-Eastern Broken Hill Block. Geological Survey of New South Wales, Bulletin 32(3), xii + 100 pp.\u003c\/p\u003e\n\u003ch4\u003e\u003cbr\u003e\u003c\/h4\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744782061726,"sku":"DRNSW_MEG_GSNSW_770","price":27.5,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/bulletin32_3_f58e43f2-5cd8-4eda-8e83-d22722758ee1.jpg?v=1773356093"},{"product_id":"771","title":"Metallogenic studies of the Broken Hill and Euriowie Blocks, New South Wales, 1988, Bulletin No. 32(1, 2)","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Broken Hill and Euriowie Blocks have been studied over more than a century mainly for Broken Hill ore bodies and the regional geology. This Bulletin summarises the regional geology, discuss past schemes used to classify mineral deposits, and provide a rationale for the classification scheme used in metallogenic studies at Broken Hill.\u003c\/p\u003e\n\u003cp\u003eMajor deposits include part of the Broken Hill Main Lode, the Pinnacles mine, the Rig Hill and Pyrite Hill cobaltiferous pyrite deposits, the Corruga calc-silicate tungsten prospects, and a wide range of vein types including the important silver-lead fields at Thackaringa and Umberumberka (Silverton).\u003c\/p\u003e\n\u003cp\u003eThe area includes most of the important deposit types found elsewhere in the Broken Hill Block except for stratabound and tin-bearing types. For each deposit or group of deposits, size, structure, mineralogy, host rocks, brief mining history and references to exploration are given. The area has been intensely explored, and has potential for deposits with commodities including lead, silver, zinc, copper, tungsten, cobalt, uranium, gold, and industrial minerals.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eBarnes R.G. 1988. Metallogenic Studies of the Broken Hill and Euriowie Blocks, New South Wales. 1.Styles of Mineralisation in the Broken Hill Block. 2. Mineral Deposits of the Southwestern Broken Hill Block. Geological Survey of New South Wales - Bulletin 32 (1,2). 250 pp.\u003c\/p\u003e\n\u003cp\u003e\u003cbr\u003e\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744782422174,"sku":"DRNSW_MEG_GSNSW_771","price":16.5,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/bulletin32_1_2_858f293a-8d99-4458-a25a-3a6856aa3801.jpg?v=1773355041"},{"product_id":"776","title":"Non-metallic and Tin Deposits of the Broken Hill District, 1982, Bulletin No. 28","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eHost rocks to the economic deposits are: mineralogically zoned granitic pegmatites (amblygonite, beryl, feldspar, mica, quartz), albite pegmatites (albite), and base metal deposits of Broken Hill, Thackaringa, and other types (fluorite and siderite). These rocks are part of the Carpentarian Willyama Complex. Other economic deposits occur within certain other rock types of the Willyama Complex such as granite gneiss (aggregate), ultrabasic rocks (asbestos), garnet-bearing schist, kyanite schist, and sillimanite schist and gneiss; dolomitic limestone has been mined from the Adelaidean Torrowangee Group. Caliche, gypsum, and sand have been mined from Quaternary deposits. Tin is included, as nearly all the tin deposits are associated with pegmatites or alluvials derived from pegmatites.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eLishmund S.R. 1982. Non-metallic and Tin Deposits of the Broken Hill District. Geological Surveyof New South Wales - Bulletin 28\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eComments\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Non-metallic and Tin Deposits of the Broken Hill District, 1982, Bulletin No. 28, also comes with an additional contents pocket.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744782454942,"sku":"DRNSW_MEG_GSNSW_776","price":19.8,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/bulletin28a.jpg?v=1773286899"},{"product_id":"1143","title":"Field Geology of New South Wales, 2000","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThis volume is an excursion guide which is aimed at giving an understanding of geological principles. This is the updated and expanded edition.\u003c\/p\u003e\n\u003cp\u003e\u003cspan\u003eNSW can be divided into 8 major geological provinces. In order of decreasing age they are: Adelaide Fold Belt, Kanmantoo Fold Belt, Lachlan Fold Belt, New England Fold Belt, Sydney-Gunnedah Basin, Clarence-Moreton Basin, Great Artesian Basin, and Murray Basin.\u003c\/span\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference \u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eBranagan D.F., \u0026amp; Packham G.H. 2000., Field Geology of New South Wales. Department of Mineral Resources New South Wales, Sydney, Australia.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eComments\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cspan style=\"color: rgb(0, 0, 0);\"\u003eA very popular introduction to the Geology of New South Wales.\u003c\/span\u003e\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744827969694,"sku":"DRNSW_MEG_GSNSW_1143","price":38.5,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/fieldgeo.jpg?v=1774302895"},{"product_id":"1159","title":"The Geological Evolution of New South Wales - A brief review","description":"\u003cp\u003e\u003cstrong\u003eComments \u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cspan\u003eThis booklet gives a summary of the geological evolution of New South Wales based on plate tectonics, and includes an overview of the plate tectonic processes. It is aimed both at geologists and at others with an interest in the topic. \u003c\/span\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cspan\u003eIt acts as a primer for the more comprehensive: Geology of New South Wales - Synthesis Volumes 1 and 2 (Memoir series, see reference list herein), and those wishing to pursue the topic further are referred to these more technical volumes.\u003c\/span\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eScheibner E. 1999. The Geological Evolution of New South Wales - A Brief Review. Geological Survey of New South Wales, Sydney. pp 31.\u003c\/p\u003e\n\u003cp\u003e\u003cbr\u003e\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744828231838,"sku":"DRNSW_MEG_GSNSW_1159","price":0.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/geologicalevolution.jpg?v=1777004118"},{"product_id":"1587","title":"Wollongong, Kiama and Robertson Explanatory Notes, 1:50,000, 1974","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe regional geology of the above mentioned 1:50,000 sheets is presented under the headings, stratigraphy and intrusives, palaeoenvironment, structural geology, hydrogeology and economic geology.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eBowman H.N. 1971. Geology of Wollongong, Kiama and Robertson 1:50,000 9029-II 9028-I\u0026amp;IV. Geological Survey of New South Wales. 219 pp.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eComments\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Wollongong, Kiama and Robertson Explanatory Notes, 1:50,000, 1974, also comes with an additional contents pocket.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744830525598,"sku":"DRNSW_MEG_GSNSW_1587","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/wollkiarobertnotes.jpg?v=1777528662"},{"product_id":"32","title":"Coastal Quaternary Geology - North and South Coast of New South Wales, 2008, Bulletin No. 34","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThis report synthesises scientific and socio-economic data about the coastal Quaternary geology of NSW to assist land-use planning and coastal management.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eTroedson A.L. and Hashimoto T.R 2008. Coastal Quaternary Geology - north and south coast of NSW. Geological Survey of New South Wales, Bulletin 34\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eComments\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eHigh-resolution (1:25,000 or better) digital mapping of the coastal Quaternary deposits of NSW was done as part of the Comprehensive Coastal Assessment. A series of 1:100,000 and 1:25,000 hard copy maps has been produced. They are double-sided and show a 1:100,000 overview of the Quaternary geology on one side. On the reverse side are two to four maps of key areas at 1:25,000.\u003c\/p\u003e\n\u003cp\u003eThe Quaternary geology was combined with existing 1:250,000 bedrock mapping, and the GIS-based map product was complemented by linked databases, such as the location of past mineral sands mining, mining and quarrying activity, field sampling data and sediment characteristics.\u003c\/p\u003e\n\u003cp\u003eThe products can assist with land-use planning and natural resource management issues - for example, in assessing geological hazards, land-use capability or finding extractive resources.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744836292766,"sku":"DRNSW_MEG_GSNSW_32","price":33.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_32.jpg?v=1593054561"},{"product_id":"541","title":"Bathurst Explanatory Notes, 1:250,000, 1998","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Bathurst 1:250,000 map sheet area in central eastern New South Wales comprises undulating hilly terrain. Largely on the western fall of the Great Dividing Range and geologically in the central eastern Lachlan Fold Belt. These explanatory notes are a product of a joint project between the Geological Survey of New South Wales and the Australian Geological Survey Organisation (AGSO) under the National Geoscience Mapping Accord.\u003c\/p\u003e\n\u003cp\u003eFor the first time in New South Wales mapping and interpretation were guided and assisted by detailed digital airborne magnetic and radiometric data. The rock units in the area have been described systematically. They record a geological history extending from the Middle Ordovician to the present, Details of the geophysical surveys are given, together with summary information on geophysical features and signatures of various rock sequences.\u003c\/p\u003e\n\u003cp\u003eMajor structural and metamorphic features have been identified. Regolith-landform features are described and their history of development discussed. Importantly, Ordovician rocks within the area are host to major Cu-Au porphyry and skarn deposit types within the map sheet area provide useful indicators for exploration.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003ePogson D.J. \u0026amp; Watkins J.J. 1998. Bathurst 1:250,000 Geological Sheet SI\/55-8: Explanatory Notes. Geological Survey of New South Wales, Sydney, xiv + 430 pp.\u003c\/p\u003e\n\u003ch4\u003e\u003cbr\u003e\u003c\/h4\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744839569566,"sku":"DRNSW_MEG_GSNSW_541","price":66.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_448.jpg?v=1593054586"},{"product_id":"560","title":"Bega-Mallacoota Explanatory Notes, 1:250,000, 1994","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThis publication is to accompany the Bega and Mallacoota 1:250,000 Geological Sheets. It serves as a compendium to illustrate and explain the geology and structural features shown in the two map sheets. The geological units in each area are described in detail covering rock units from Cambro-Ordovician age to Canozoic volcanics and sediments.\u003c\/p\u003e\n\u003cp\u003eThe structural geology of different lithotectonic units, style and geometry of structural zones, together with cross faults and megakinks are described.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eLewis P.C., Glen R.A., Pratt G.W. \u0026amp; Clarke I., 1994. Bega-Mallacoota 1:250,000 Geological Sheet SJ\/55-4, SJ\/55-8 Explanatory Notes, 148 pp, 8 pls. Geological Survey of New South Wales, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744841076894,"sku":"DRNSW_MEG_GSNSW_560","price":22.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_449.jpg?v=1593054593"},{"product_id":"745","title":"Taralga Explanatory Notes, 1:100,000, 1970","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Taralga 1:100,000 sheet covers some 2,650 square km of the Central Highlands of New South Wales between Oberon and Goulburn, and is occupied by rocks ranging in age from Ordovician to recent.\u003c\/p\u003e\n\u003cp\u003eThe geological map was compiled on the basis of about 25 weeks of field mapping on aerial photographs, and weeks of photo interpretation, taking into account and using all available data resulting from previous studies, either published or unpublished. The petrographic descriptions were done by J.Watts and L.Stevenson, and the paleontological determination by J.Pickett and L.Sherwin.\u003c\/p\u003e\n\u003cp\u003eIn presenting the Taralga geological sheet and explanatory notes, it is apparent that many problems are still unresolved and unexplained. However, a certain stage of knowledge has been reached and the main problems delineated. It is considered that further detailed mapping and special investigations are necessary in some areas.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eScheibner E., 1970. Geology of the Taralga 1:100,000 Sheet 8829. Geological Survey of New South Wales, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744865587358,"sku":"DRNSW_MEG_GSNSW_745","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/taralgaexplannotes.jpg?v=1776992900"},{"product_id":"750","title":"Yass Explanatory Notes,  1:100,000, 1978","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Yass 1:100,000 sheet covers an area of about 2600 square km, and is located about 320 Km southwest of Sydney in the fertile grazing country of the southwestern slopes of New South Wales. Steeply dipping slates of Ordovician age (Jerrawa Beds) are the oldest rocks found in the area. Theses rocks are overlain, with apparent unconformity, by the Mundoonen Sandstone of Silurian age. The Douro Group, a thick sequence consisting dominantly of tuffs and volcanics, overlies this formation and covers about 60 per cent of the map area. The almost complete absence of bedding in these rocks makes the study of their geological structure very difficult.\u003c\/p\u003e\n\u003cp\u003eThe overlying Laidlaw and Silverdale Formations and Booroo Ponds and Barambogie Groups consist of a fossiliferous sequence of sediments, with shales and limestones dominant. This sequence is limited in areal extent to the Yass Basin. The Black Range Group, a dominantly volcanic sequence, is of Early Devonian age. Mapping of the Kirawin Shale within this sequence in the Burrinjuck Dam area has outlined a number of fold structures. The Murrumbidgee Group overlies the Black Range Group and consists dominantly of complexly folded fossiliferous limestones. Granitic rocks intrude the Silurian sequence, but their outcrop occupies only a relatively small proportion of this sheet.\u003c\/p\u003e\n\u003cp\u003eThe Geological Survey of New South Wales 1:100,000 mapping programme covers areas of special geological or mineral resource interest within New South Wales. The Yass sheet contains the Yass and Taemas area, which have come to be regarded as classic for the study of Silurian and Devonian sedimentation on the stare.\u003c\/p\u003e\n\u003cp\u003eA considerable amount of stratigraphic and paleontological information has been published on these areas and they have been visited by students of geology for many years.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eCramsie J.N., Pogson D.J., and Baker C.J., 1978. Geology of the Yass 1:100,000 Sheet 8628. New South Wales Geological Survey, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744865620126,"sku":"DRNSW_MEG_GSNSW_750","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/yassnotes.jpg?v=1777603651"},{"product_id":"1547","title":"Goulburn Explanatory Notes, 1:250,000, 2011","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Goulburn 1:250,000 map sheet area (lies largely within the Southern Highlands of eastern New South Wales, and is centred about 170 km southwest of Sydney and 80 km north of Canberra. This area is subject to increasing land use pressure, with demand for industrial sites adjacent to existing infrastructure and for semi-rural residential blocks.\u003c\/p\u003e\n\u003cp\u003e\u003cspan style=\"font-size: 0.875rem;\"\u003eThe Goulburn area is an important supplier of extractive minerals for the expanding metropolitan areas, agriculture and metalliferous mining. The Goulburn Mapping Project has provided detailed up-to-date geoscientific data to assist mineral exploration and resource identification and will contribute to informed land use decisions in the future. These explanatory notes provide a detailed description of all lithostratigraphic and plutonic units, the structural and metamorphic framework and a synthesis of the geological history and major mineral systems of goulburn250.\u003c\/span\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cspan style=\"font-size: 0.875rem;\"\u003eThis publication accompanies a series of six detailed 1:100,000 surficial geology maps (including Cainozoic cover), one detailed 1:50,000 geology map of the Yass Basin area, and the second edition 1:250,000 solid (basement) geology map. This work is supported by high-resolution airborne radiometric, magnetic and digital elevation data, and a 4 km x 4 km regional gravity grid. \u003c\/span\u003e\u003cspan style=\"font-size: 0.875rem;\"\u003eThe map sheet area lies in a relatively well-exposed region of the eastern Lachlan Orogen which developed at the convergent eastern margin of the Gondwana Craton during the Ordovician to Carboniferous. \u003c\/span\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cspan style=\"font-size: 0.875rem;\"\u003eThe orogen developed through several cycles of sedimentation, volcanism and plutonism, generally related to crustal extension associated with subduction, separated by relatively short-lived compressional orogenic events. Overlying Permian rocks of the subsequent Sydney Basin crop out near the eastern edge of the area and Cainozoic basalt and unconsolidated sedimentary deposits locally mask the older sequences.\u003c\/span\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThomas O.D. \u0026amp; Pogson D.J. (compilers) 2012. Goulburn 1:250,000 Geological Sheet SH\/55-12, 2nd edition, Explanatory Notes. Geological Survey of New South Wales, Maitland, NSW.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744866799774,"sku":"DRNSW_MEG_GSNSW_1547","price":37.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_650.jpg?v=1774404848"},{"product_id":"718","title":"Camberwell, Dungog \u0026 Bulahdelah Explanatory Notes, 1:100,000, 1991","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe regional geology of the Camberwell, Dungog and Bulahdelah 1:100,000 map sheet areas covers mainly Palaeozoic (Devonian to Permian) rocks and the Quaternary igneous and sedimentary units (especially coastal sediments). Discussion is based in part on geophysical studies. Figures, especially stratigraphic columns, and Photographs and other data support the discussion. The area covered by these three maps includes much of the northeastern part of the Sydney Basin, the Gloucester Basin and Cranky Corner Basin and adjacent rocks of the Tamworth Belt. The older rocks (Tamworth Belt) are Devonian to Carboniferous, there being (in these Notes) limited definition of the boundary. Those rocks are, structurally, separated from the Sydney Basin by the Hunter Fault (or Thrust). The Cranky Corner Basin, with rocks to Permian age, rests (perhaps with conformity) on Tamworth Belt units.\u003c\/p\u003e\n\u003cp\u003eSimilarly, the Gloucester Basin includes Permian rocks, including important coal-bearing units. Discussion in the Notes is centred on structural blocks. Those blocks are, from west to east: Rouchel Block; Gresford Block; Western Myall Block; and Eastern Myall Block. The structure and structural history of those blocks include extensive folding and faulting with broadly north-south trends. Rocks of the Rouchel Block are mainly Devonian (Goonoo Goonoo Mudstone) and Carboniferous marine (with transgressive and regressive episodes) sedimentary units with some extensive volcanic influences. Rocks (Carboniferous) of the Gresford Block are similar, with significant volcanic units, with the Carboniferous to Permian section of the Cranky Corner basin containing some coals.\u003c\/p\u003e\n\u003cp\u003eRocks of the Myall blocks also include correlative Devonian to Carboniferous sections - with the important younger Permian section in the Gloucester Basin including well-developed coal units - albeit with noticeable tilting of the coal in places.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eRoberts, J., Engel, B., and Chapman, J., 1991. Geology of the Camberwell, Dungog, and Bulahdelah 1:100,000 Sheets 9133, 9233, 9333. 382 pp. New South Wales Geological Survey , Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744869421214,"sku":"DRNSW_MEG_GSNSW_718","price":22.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/camberwellnotes.jpg?v=1773366206"},{"product_id":"1578","title":"Sussex-Byrock Explanatory Notes 1:100,000, 2012","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Sussex and Byrock 1:100,000 geological sheets 8135 and 8136, Explanatory Notes is a full colour book which will accompany the Sussex and Byrock geological 1:100,000 map sheets of areas to the east of Cobar. The explanatory notes include chapters describing rock units, structure and metamorphism, mineral systems, geophysics and a geological synthesis.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eBurton G.R. Trigg S.J. Campbell L.M. 2012. Sussex and Byrock 1:100,000 Geological Sheets 8135 and 8136. Explanatory Notes. Geological Survey of New South Wales. Maitland. 173pp.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744872370334,"sku":"DRNSW_MEG_GSNSW_1578","price":40.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/sussexbyrock.jpg?v=1776897471"},{"product_id":"563","title":"Cargelligo Explanatory Notes, 1:250,000, 2005","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Cargelligo 1:250,000 map sheet area is located in central New South Wales, approximately 550 km west of Sydney. The map area contains a poorly exposed sequence of the central Lachlan Orogen, consisting of Ordovician to Devonian volcanic, sedimentary and plutonic rocks. Tertiary to Quaternary deposits of the eastern Murray Basin onlap the Palaeozoic sequences in the west of the map area and minor Tertiary volcanic units are present in the east of the map area. Widespread unconsolidated Quaternary deposits cover much of the older sequences.\u003c\/p\u003e\n\u003cp\u003eRemapping of the Cargelligo 1:250,000 map sheet area, aided by airborne geophysical data, has enhanced understanding of the stratigraphy, structure, mineral potential and evolution of the central Lachlan Orogen. High-quality aeromagnetic, radiometric and gravity data has enabled further investigation of the generally poorly -outcropping rocks in the area. The early Palaeozoic bedrock is divided into two major structural zones east and west of the Bootheragandra Fault: the Wagga-Omeo Zone to the east and the Howqua Zone to the west.\u003c\/p\u003e\n\u003cp\u003eYounger Siluro-Devonian volcanic rocks and sedimentary rocks combine to form the southern part of the Darling Zone - including the Mount Hope Trough, Rast Trough, the Walters Range Shelf and Melrose Trough. Structures in Late Devonian fluvial basins are superimposed on the previously deformed basement and are included in the Cocoparra, Narriah and Lachlan Range Synclines.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eColquhoun G.P., Meakin N.S. \u0026amp; Cameron R.G. (compilers) 2005. Cargelligo 1:250,000 Geological Sheet SI\/556, 3rd edition, Explanatory Notes. Geological Survey of New South Wales, Maitland, NSW, 291 pp.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744878432414,"sku":"DRNSW_MEG_GSNSW_563","price":66.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_451.jpg?v=1593054689"},{"product_id":"565","title":"Dubbo Explanatory Notes 1:250,000, 1999","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eExplanatory notes on the Dubbo 1:250,000 map sheet area are compiled in this report. The area is located 250 km north-west of Sydney and includes the exposed north-eastern portion of the Palaeozoic Lachlan Orogen and overlying marginal areas of the Permo-Triassic Sydney-Gunnedah Basin and Jurassic Surat basin.\u003c\/p\u003e\n\u003cp\u003eThe stratigraphic sequence of the Lachlan orogen have been deformed into meridional structural packages (fold or thrust sheets). Regional metamorphism ranges from zeolite\/clay\/carbonate to actinolite\/biotite grade. The stratigraphy, structure, geophysics, mineralogy (mineral occurrences), palaeontology and coal measures of the area are discussed in this report.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eMeakin N.S. and Morgan E.J. (compilers) 1999. Dubbo 1:250,000 Geological Sheet SI\/55-4, 2nd Edition. Explanatory Notes. Geological Survey of New South Wales, Sydney, xvi + 504 pp.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744884035742,"sku":"DRNSW_MEG_GSNSW_565","price":82.5,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/dubboexplannotes.jpg?v=1773890977"},{"product_id":"731","title":"Cootamundra Explanatory Notes, 1:100,000, 1975","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Cootamundra 1:100,000 sheet covers and area of approximately 2,500 km2 in the south eastern part of the New South Wales, on the western slopes of the Great Dividing Range.\u003c\/p\u003e\n\u003cp\u003eThe area includes the major part of County Harden, and small parts of Counties Bland, Buccleuch, and Clarendon. The area covered by the Cootamundra 1:100,000 sheet is in the southern part of the Lachlan Fold belt which developed from the Palaeozoic Lachlan Mobile Zone. The Lachlan Fold Belt has been subdivided into several north-south trending anticlinorial and synclinorial zones (Scheibner 1972b).\u003c\/p\u003e\n\u003cp\u003eThe Cootamundra sheet straddles the southern part of the Forbes Anticlinorial Zone, and covers part of the Bogan Gate Synclinorial Zone on the west and the Cowra-Yass Synclinorial Zone on the east.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eBasden H., Adrian J., Clift D.S.L, \u0026amp; Winchester R.E. 1975. Geology of the Cootamundra 1:100,000 Sheet 8528. Geological Survey of New South Wales, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744884199582,"sku":"DRNSW_MEG_GSNSW_731","price":11.55,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/cootamundranotes.jpg?v=1773785840"},{"product_id":"775","title":"Manilla 1:100,000 Explanatory Notes, 2010","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Manilla 1:100,000 map sheet area (Manilla) includes rocks of the Tamworth Belt and Central Block of the New England Orogen, which are separated by the Peel Fault. Each block is characterised by its own unique assemblage of rock types, structures, tectonostratigraphic terranes and mineralisation.\u003c\/p\u003e\n\u003cp\u003eThe Tamworth Belt contains Early Devonian to Late Carboniferous regressive marine to non-marine sequence of sedimentary and minor volcanic rocks. Most of these rocks make up the Gamilaroi terrane. The strata reflect a change from basal slope marine sedimentation through shelfal deposition, near-shore and shoreline marine, and ultimately continental fluvial and glacigene sedimentary and volcanic deposition. Olistostromal sedimentary and volcanic rocks are common throughout the marine strata, representing environments that were proximal to steep slopes, deeply incised submarine canyons, and island-arc flanks.\u003c\/p\u003e\n\u003cp\u003eThe rocks show an evolution from andesitic and some basaltic volcanism in the Devonian and Early Carboniferous to rhyolitic and rhyodacitic volcanism in the Late Carboniferous. In Manilla, the Tamworth Belt is subdivisible into a number of structural domains characterised by distinctive structural suites. These domains increase in complexity eastward towards the Peel Fault. Low bedding dips, open first-generation folds with open second-generation cross folds and low-angle, bedding-parallel thrusts characterise the west of the area. Vertical and overturned bedding, accompanied by first-generation tight folds, second-generation isoclinal folds with well-developed slaty cleavage and folded, steeply dipping thrusts characterise the rocks adjacent to the Peel Fault.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eVickery N.M., Brown R.E. \u0026amp; Percival, I.G. (compilers) 2010. Manilla 1:100,000 Geological Sheet 9036, Explanatory Notes. Geological Survey of New South Wales, Maitland.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744886853790,"sku":"DRNSW_MEG_GSNSW_775","price":60.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_653.jpg?v=1593054721"},{"product_id":"736","title":"Michelago Explanatory Notes, 1:100 000, 1979","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Michelago 1:100,000 sheet covers an area of some 2497 square km in the State of New South Wales and the southeast portion of the Australian Capital Territory. The Michelago 1:100,000 sheet belongs structurally to the southern portion of the Lachlan Fold Belt.\u003c\/p\u003e\n\u003cp\u003eThis fold belt forms part of the Tasman Fold Belt System, and its origins can be traced back to the Cambrian period. Three main structural zones are recognised within the area. These are the Cowra-Yass Synclinorial Zone, the Captains Flat-Goulburn Synclynorial Zone, and the Molong-South Coast Anticlinorial Zone with Late Ordovician rocks representing the oldest in the area.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eRichardson S.J., 1979. Geology of the Michelago 1:100,000 Sheet 8726. New South Wales Geological Survey, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744887378078,"sku":"DRNSW_MEG_GSNSW_736","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/michelagonotes.jpg?v=1775093865"},{"product_id":"738","title":"Narooma Explanatory Notes, 1:100,000, 1977","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eDetailed regional stratigraphic geology of the Narooma 1:100,000 sheet is described. Mining history of gold and phosphate deposits is given briefly. The Narooma 1:100,000 Geological Sheet covers a land area of 575 km2, the remaining 1,900 square km being over the Tasman Sea.\u003c\/p\u003e\n\u003cp\u003eThe Palaeozoic and Mesozoic geology of this sheet was mapped and compiled by L.E. Chalker during 1970. Her accompanying notes were subsequently updated in June 1975, prior to publication, by D.J. Pogson from additional publishes and unpublished thesis work.\u003c\/p\u003e\n\u003cp\u003eThe Tertiary, Quaternary, and offshore geology sections are based on field observation and on collation and interpretation of offshore data by C.S. Bembrick during the period 1968 - 1975.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eChalker L.E. \u0026amp; Bembrick C.S., 1997. Geology of the Narooma 1:100,000 Sheet 8925. Geological Survey of New South Wales, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744889016478,"sku":"DRNSW_MEG_GSNSW_738","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/naroomanotes.jpg?v=1776224183"},{"product_id":"741","title":"Numbla Explanatory Notes, 1:100,000, 1989","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Numbla 1:100,000 sheet covers an area of 2650 square km in the southernmost part of the Southern Tablelands of New South Wales. About 70 square km of the south-western corner of the sheet is in the State of Victoria.\u003c\/p\u003e\n\u003cp\u003eThe area covered by the Numbla sheet is on the southern part of the Palaeozoic Lachlan Fold Belt (Scheibner 1973), or the Lachlan Geosyncline of Packham (1960).\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eWhite, A.J.R., and Chappell, B.W., 1989. Geology of the Numbla 1:00,000 Sheet 8624. 160 pp. New South Wales Geological Survey, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744890097822,"sku":"DRNSW_MEG_GSNSW_741","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/numblanotes.jpg?v=1776313582"},{"product_id":"743","title":"Penrith Explanatory Notes, 1:100,000, 1991","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThese notes accompany the Penrith 1:100,000 geological map sheet. The area described in the map and notes is in western Sydney and is thus important - with conflicting land use pressures. Appendixes include information on geophysical surveys and boreholes.\u003c\/p\u003e\n\u003cp\u003eThe geology in the Penrith 1:100,000 map sheet area occupies a roughly central position in the Sydney Basin. Rocks in the eastern part of the map area have relatively flat dips but the western part of the area includes the relatively steep dips associated with the Lapstone Monocline\/Nepean Fault and Kurrajong Fault - separating the Cumberland Plain from the Blue Mountains Plateau. Although the Permian (and possibly latest Carboniferous) rocks of the Sydney Basin are present at depth and have coal and gas potential, the Triassic section is the main part preserved in the Penrith area.\u003c\/p\u003e\n\u003cp\u003eRocks of the upper part of the Narrabeen Group, Hawkesbury Sandstone, (Mittagong Formation) and the Wianamatta Group have been mapped in the area - the Wianamatta Group being the most important (near-) surface unit (albeit with relatively poor outcrop characteristics). The rocks are mainly sandstones and shales of lacustrine origin. Younger units are Mesozoic (mainly) intrusions - especially the Prospect Picrite, diatremes and dykes. Cainozoic units include poorly consolidated sediments (some coarse, and some extensive).\u003c\/p\u003e\n\u003cp\u003eResource exploitation has been extensive: coarse aggregate; fine aggregate; clay\/shale; etc. Much of that material has either been worked out or is now unavailable. Soils and groundwater are also important resources in the area. Both natural and man-induced engineering factors and environmental considerations form part of the discussion - important in an area of riverine plains and extensive urbanisation.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eJones D.C., and Clark N.R., (eds), 1991. Geology of the Penrith 1:100,000 Sheet 9030. 201 pp. New South Wales Geological Survey, Sydney.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34744890622110,"sku":"DRNSW_MEG_GSNSW_743","price":22.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/penrithnotes.jpg?v=1776386261"},{"product_id":"767","title":"Industrial Mineral Opportunities in New South Wales, 2007, Bulletin No. 33","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThis bulletin describes the occurrence and geological setting of industrial minerals in New South Wales, and exploration potential for them. The research updates previous studies by the Geological Survey of New South Wales and is designed to encourage additional exploration and development of the states industrial minerals.\u003c\/p\u003e\n\u003cp\u003eThe bulletin has substantially enhanced understanding of industrial mineral occurrences in New South Wales and has the potential to provide industrial mineral explorers with a distinct advantage in the search for new deposits. New South Wales contains outcropping rocks ranging in age from Palaeoproterozoic to Recent that formed in a diverse array of geological settings. \u003c\/p\u003e\n\u003cp\u003eMany of these rocks have an extensive regolith cover extending to alluvial deposits, sand dunes, inland salt lakes, deep weathering profiles and thick soils. These sequences have given rise to a considerable range of industrial minerals that make an important contribution to the economy and form a diverse sector of the states minerals industry.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eWhitehouse J., Brownlow J.W., Burton G.R., Ferguson A.C., Glen R.A., Lishmund S.R., MacRae G.P., Malloch K.R., Oakes G.M., Paterson I.B.L., Pienmunne J.T., Ray H.N. \u0026amp; Watkins J.J. 2007. Industrial Mineral Opportunities in New South Wales. Geological Survey of New South Wales, Bulletin 33.\u003cstrong\u003e\u003c\/strong\u003e\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34745064456350,"sku":"DRNSW_MEG_GSNSW_767","price":44.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_654.jpg?v=1593055120"},{"product_id":"772","title":"Contributions to the Geology of Great Australian Basin in New South Wales, 1984, Bulletin No. 31","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe selection and correlation of zones of characteristic gamma ray deflection in the Great Australian in NSW yielded two related systems of zones - one for the eastern part of the basin and for the west. The gamma ray logs alone cannot be easily interpreted in terms of lithology as the basin contains unusual clay mineral assemblages which greatly affect the gamma radiation emitted by a rock unit.\u003c\/p\u003e\n\u003cp\u003eA relationship between the known lithologies and the gamma ray correlation zones has however been established and the gamma ray correlation can be used to extrapolate lithological information from control boreholes to other boreholes for which only gamma ray logs are available. The cuttings lithological logs and geophysical logs from the Lightning Ridge Town Water Supply bore and exploratory petroleum wells do however provide additional control. \u003c\/p\u003e\n\u003cp\u003eThe lack of data in the transition between the eastern and western areas prevents a good understanding of the E-W relationships. Some correlations can be inferred between the upper parts of the sequences in both areas. It should be noted that the areal distribution of available gamma ray logs is such that very detailed correlations could be attempted only in some localised parts of the basin.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eHawke J.M. and Cramsie J.N. 1984. Contributions to the Geology of the Great Australian Basin in New South Wales. Geological Survey of New South Wales - Bulletin 31.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34745066094750,"sku":"DRNSW_MEG_GSNSW_772","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/bulletin31.jpg?v=1773354797"},{"product_id":"774","title":"The Silurian System in New South Wales, 1982, Bulletin No. 29","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Silurian System in New South Wales covers detailed descriptions of the Palaeogeographic and Stratigraphic History, Biostratigraphy, Stratigraphic Units and Intrusive Units. Palaeogeographic and Stratigraphic History provides detail of the following; Basement materials, Llandovery, Early \u0026amp; Late Wenlock, Ludlow and Pridoli. Biostratigraphy detail includes; Rugose corals, Tabulate corals, Conodonts, Graptolites, Brachiopods, Trilobites, Stramatoporoids and Microplankton.\u003c\/p\u003e\n\u003cp\u003eThe Stratigraphic Units consist of the Girilambone - Wagga Anticlinorial Zone and Cobar Synclinorial Zone, Mineral hill Synclinorial Zone, Bogan Gate Synclinorial Zone, Forbes Anticlinorial Zone, Cowra - Yass Synclinorial Zone, Molong - South Coast Anticlinorial Zone, Hill End Synclinorial Zone, captains Flat - Goulburn Synclinorial Zone and the New England Area. Intrusive units are also in great detail.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003ePickett J. 1982. The Silurian System in New South Wales. Geological Survey of New South Wales, Bulletin 29.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eComments\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Silurian System in New South Wales, 1982, Bulletin No. 29, also comes with an additional contents pocket.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34745066586270,"sku":"DRNSW_MEG_GSNSW_774","price":15.95,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/bulletin29a.jpg?v=1773287590"},{"product_id":"777","title":"Eustasy in the Australian Early and Middle Cretaceous, 1980, Bulletin No. 27","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eCretaceous biostratigraphy of the Eromanga enabled correlation within the Great Australian Basin and with other basins in Australia. Comparison of the Australian sea level curve with other structurally simple intracratonic basins worldwide showed that these events were eustatic. The mechanism during eustatic changes in sea level is not yet fully understood, but may be related to changing rates of sea floor spreading.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eMorgan R. 1980. Eustasy in the Australian Early and Middle Cretaceous. Geological Survey of New South Wales - Bulletin 27\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34745066913950,"sku":"DRNSW_MEG_GSNSW_777","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/bulletin27.jpg?v=1773286058"},{"product_id":"779","title":"The Geology and resource potential of the Wianamatta group, 1979, Bulletin No. 25","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Wianamatta Group, of Middle Triassic age, is the topmost Mesozoic unit in the Sydney Basin. Three formations are recognized. The Ashfield Shale, 45 to 60 m thick, comprises a dark grey to black siltstone which grades upwards into a laminite. The overlying, thin, quartz lithic Minchinbury Sandstone is less than 4 m thick. The Bringelly Shale comprises 257 m of mainly claystone and siltstone with laminite, sandstone, carbonaceous claystone, and rare coal. The Wianamatta Group was deposited during a single regressive episode. The sequence grades upwards from a lacustrine to a marine or brackish facies, (Ashfield Shale), through a shoreline facies comprising a beach and barrier bar complex (Minchinbury Sandstone), into an over-lying lagoonal marsh facies which grades up into an alluvial or estuarine coastal plain facies (Bringelly Shale). The Wianamatta Group is the chief source of raw material for the production of structural bricks in the Sydney Region. Both the Ashfield Shale and the Bringelly Shale possess the ability to bloat and have potential for the production of lightweight expanded aggregate.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eHerbert C. 1979. The Geology and Resource Potential of the Wianamatta Group. Geological Survey of New South Wales - Bulletin 25\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34745068519582,"sku":"DRNSW_MEG_GSNSW_779","price":11.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/files\/bulletin25.jpg?v=1773282579"},{"product_id":"804","title":"Bulletin of the Coalfield Geology Council of New South Wales, 1999, Bulletin No. 1","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eContains computer-based resource\/reserve estimates; guide to systematic evaluation of open cut coal reserves; environmental considerations for coal geologists; Permian stratigraphy of the Gunnedah Basin; stratigraphy of the Greta Coal Measures, Muswellbrook Anticline area, Hunter Coalfield; coal seam nomenclature application in the Hunter Coalfield; revised stratigraphy of the Newcastle Coal Measure; Southern Coalfield stratigraphy and terminology.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eCoalfield Council of New South Wales. 1999. Bulletin of the Coalfield Geology Council of New South Wales, Bulletin 1.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eComments\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003e\u003cspan\u003ePublication is now out of print. \u003c\/span\u003e\u003cspan\u003eDigital copies of the book can now be found and downloaded on DIGS.\u003cbr\u003e\u003c\/span\u003e\u003ca href=\"https:\/\/search.geoscience.nsw.gov.au\/product\/692\" rel=\"noopener\" target=\"_blank\"\u003e\u003cspan\u003ehttps:\/\/search.geoscience.nsw.gov.au\/product\/692\u003c\/span\u003e\u003c\/a\u003e\u003cbr\u003e\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34745071009950,"sku":"DRNSW_MEG_GSNSW_804","price":33.0,"currency_code":"AUD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_692.jpg?v=1593055132"},{"product_id":"807","title":"New South Wales Petroleum Potential, 1995, Bulletin No. 1","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThis publication was prepared by the Government and the Department of Mineral Resources to highlight the petroleum potential of NSW to explorationists. This book gives an overview of the hydrocarbon prospectively of the seven main sedimentary basins in NSW i.e. Clarence-Moreton, Darling, Eromanga, Gunnedah, Murray, Surat and Sydney Basins.\u003c\/p\u003e\n\u003cp\u003eThe overview provides information regarding location, geological setting, structural setting, exploration history, stratigraphy and depositional setting. Occurrence of hydrocarbon, structure, reservoir potential, source rocks, exploration potential, play fairways, Oil shales and coal seam methane potential are also discussed for these basins.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eStewart J.R. \u0026amp; Alder J.D. eds 1995. New South Wales Petroleum Potential, New South Wales Department of Mineral Resources, Sydney, 188 pp.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34745071304862,"sku":"DRNSW_MEG_GSNSW_807","price":99.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_695.jpg?v=1593055134"},{"product_id":"16","title":"Explanatory notes for the Koonenberry Belt Geological Maps, 2010, Bulletin No. 35","description":"\u003cp\u003e\u003cstrong\u003eAbstract\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Koonenberry Belt in the far northwestern area of New South Wales (north-northeast of the internationally renowned mining centre of Broken Hill) forms a significant segment of the Cambrian Delamerian Orogen that developed along the eastern margin of the AustralianAntarctic continent following the late Proterozoic Rodinian break-up and the birth of the Proto-Pacific Ocean. Following the Delamerian Orogeny, the belt has undergone a rich history of multiple uplift, sedimentation and deformation throughout the Phanerozoic.\u003c\/p\u003e\n\u003cp\u003eThe Koonenberry Belt is prospective for a range of commodities including gold, copper and nickel and is underexplored by modern exploration methods. Since 1995 the Koonenberry Belt has been a focus of investigation by the Geological Survey of New South Wales. Regional geological mapping was undertaken throughout the belt following acquisition of highresolution geophysical data and a deep seismic reflection survey, funded by New South Wales Government initiatives including Discovery 2000, Exploration NSW and New Frontiers.\u003c\/p\u003e\n\u003cp\u003eIn addition, NSW Department of Primary Industries staff worked within the former CRC LEME (Cooperative Research Centre for Landscape Environments and Mineral Exploration) to conduct numerous regolith and baseline geochemistry studies in the Koonenberry Belt area. The outcomes of this regional mapping and research include major advancements in the understanding of the geological history of the Koonenberry Belt. A total of 497 units have been mapped, including 72 new, formally defined units.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eReference\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eGreenfield J.E., Gilmore P.J. \u0026amp; Mills K.J. (compilers). 2010. Explanatory notes for the Koonenberry Belt geological maps. Geological Survey of New South Wales, Bulletin 35.\u003c\/p\u003e\n\u003cp\u003e\u003cstrong\u003eComments\u003c\/strong\u003e\u003c\/p\u003e\n\u003cp\u003eThe Koonenberry Belt in northwestern NSW is prospective for a range of commodities - gold, copper and nickel - and is underexplored by modern exploration methods. GSNSW conducted regional geological mapping following acquisition of high resolution geophysical data and a deep seismic reflection survey as well as regolith and baseline geochemistry studies.\u003c\/p\u003e\n\u003cp\u003e497 units have been mapped, including 72 new, formally defined units. The Bulletin accompanies 22 geological maps (12 x 1:100,000 and 4 x 1:25,000 geological maps; 2 x 1:250,000 solid geology interpretation maps and 4 x 1:100,000 regolith maps). A DVD of the data is included.\u003c\/p\u003e","brand":"Geological Survey of New South Wales","offers":[{"title":"Default Title","offer_id":34745088737438,"sku":"DRNSW_MEG_GSNSW_16","price":150.0,"currency_code":"AUD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/products\/DRNSW_MEG_GSNSW_17.jpg?v=1593055200"}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0413\/1530\/3582\/collections\/Untitled_d3ec0678-1179-4e07-a96f-da715f1514b8.png?v=1592265096","url":"https:\/\/shop.regional.nsw.gov.au\/collections\/books\/scale-1-50000.oembed","provider":"Regional NSW","version":"1.0","type":"link"}