Thematische Bibliographien / Geology Australia

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Auswahl der wissenschaftlichen Literatur zum Thema „Geology Australia“

Autor: Grafiati

Veröffentlicht am 4. Juni 2021

Zuletzt aktualisiert am 28. Juli 2024

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Zeitschriftenartikel zum Thema "Geology Australia"

Lewis, Ian D. „Evolution of Geotourism in Australia from Kanawinka Global Geopark and Australian National Landscapes to GeoRegions and Geotrails: A Review and Lessons Learned“. Land 12, Nr. 6 (06.06.2023): 1190. http://dx.doi.org/10.3390/land12061190.

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The geological heritage of Australia’s landscapes and World Heritage areas has generally been underpromoted to the public by the tourism industry. However, in 2008, the fledgling world of geotourism in Australia received a significant boost with two events: the Inaugural Global Geotourism Conference ‘Discover the Earth beneath our Feet’ held in Fremantle, Western Australia, and the declaration of the UNESCO Kanawinka Global Geopark, which linked volcanic regions in South Australia and Victoria. Simultaneously the Australian Federal Government launched the ‘Australian National Landscapes’ (ANL) program. However, this impetus was not sustained when the Kanawinka Global Geopark was deregistered as a UNESCO-branded geopark in 2012, and the ANL program faded within a decade. Despite these setbacks, as an outcome of the 2008 Fremantle conference, several productive lines of geotourism have developed across Australia. This paper reviews the history of Australian geotourism since 2008. It examines the impacts of the experiences, lessons learned, problems for geology as perceived by National Parks and the Environment movement, geological communication problems, and the subsequent evolution of Australian geotourism. From these issues, new non-government bodies and initiatives have arisen, including the Australian Geoparks Network, the Australian Geoscience Council, and the recent development of a National Geotourism Strategy. Strong elements emerging from these initiatives are the increasing development of geotrails (which suit the large Australian continent) and the new Australian concept of ‘GeoRegions’. These are in response to an awareness that geotourism requires a flexible outlook to widen the appreciation and appeal of geological heritage and landscapes to the broader public. A further new direction is suggested: for Australian geotourism to combine with some elements of ICOMOS Cultural Routes. An outstanding example, the ICOMOS Overland Telegraph Line (OTL) Cultural Route that crosses Australia from south to north, is considered. For 2000 km, the construction of this line in the 1870s followed the regional geology and hydrology, relying upon the available biota but bringing about a clash of human cultures. The six colonies of Australia were finally linked to the world by wire, but the arrival of the OTL had a significant impact on the country’s Indigenous inhabitants. In Australia and globally, geotourism is incorporating the A–B–Cs (abiotic, biotic and cultural elements) to more effectively encourage the public to value their landscapes and the associated stories. The OTL provides an example of a newly introduced fourth dimension for geotourism, which gives consideration to the socio-political context of landscape adaptation.

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Plumb, K. A. „Proterozoic geology of Australia and palaeomagnetism“. Exploration Geophysics 24, Nr. 2 (Juni 1993): 213–18. http://dx.doi.org/10.1071/eg993213.

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Groves, David I., Mark E. Barley und Julie M. Shepherd. „Geology and Mineralisation of Western Australia“. Exploration Geophysics 25, Nr. 3 (September 1994): 163. http://dx.doi.org/10.1071/eg994163.

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Nott, Jonathan F. „The urban geology of Darwin, Australia“. Quaternary International 103, Nr. 1 (Januar 2003): 83–90. http://dx.doi.org/10.1016/s1040-6182(02)00143-x.

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Cook, Robert B. „Ataeamite: Moonta Mine, South Australia, Australia“. Rocks & Minerals 81, Nr. 5 (Januar 2006): 374–78. http://dx.doi.org/10.3200/rmin.81.5.374-378.

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Jworchan, Indra, Tony O' Brien, Emged Rizkalla und Paul Gorman. „Engineering geology of Waterside Green, Sydney, Australia“. Journal of Nepal Geological Society 34 (09.10.2006): 53–62. http://dx.doi.org/10.3126/jngs.v34i0.31879.

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Development of low-lying land affected by high water table in saline and sodic soils and local swampy areas remains a challenge for the local government, developers, and other regulators. The development control plan for a proposed residential or commercial subdivision in such a site in Penrith, Sydney, Australia, states that the drainage and stormwater management systems within and across the site should be improved and proposed buildings should be constructed on the ground higher than the 100-year flood level. This paper presents the results of engineering geological and geotechnical investigations for the proposed subdivision. The subsurface profile at the site comprises alluvial deposits underlain by residual soil, which in turn is underlain by shale and sandstone. In the eastern portion of the site, the alluvial deposits comprise a sequence of clay, sand and gravel, and in the western portion they contain a succession of clean sand and gravel. The alluvium in the eastern portion of the site is saline whereas it is generally non-saline in the western portion. All saline soils are sodic and most non saline ones are non-sodic. This paper discusses the suitability of on-site soils for use in a structural fill and impermeable clay liner as well as the management of saline and dispersive soils.

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Nott, Jonathan F. „The urban geology of Cairns, Queensland, Australia“. Quaternary International 103, Nr. 1 (Januar 2003): 75–82. http://dx.doi.org/10.1016/s1040-6182(02)00142-8.

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Groves, David I., Mark E. Barley und Julie M. Shepherd. „OVERVIEWS: Geology and mineralisation of Western Australia“. ASEG Extended Abstracts 1994, Nr. 1 (Dezember 1994): 1–28. http://dx.doi.org/10.1071/asegspec07_02.

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McNally, G. H. „Some issues in environmental geology in Australia“. Australian Journal of Earth Sciences 47, Nr. 1 (Februar 2000): 1. http://dx.doi.org/10.1046/j.1440-0952.2000.00767.x.

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Kear, B. P., J. A. Long und J. E. Martin. „A review of Australian mosasaur occurrences“. Netherlands Journal of Geosciences 84, Nr. 3 (September 2005): 307–13. http://dx.doi.org/10.1017/s0016774600021089.

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AbstractMosasaurs are rare in Australia with fragmentary specimens known only from the Cenomanian-lower Turonian Molecap Greensand (Perth Basin), Campanian - lower Maastrichtian Korojon Calcarenite (Carnarvon Basin), and upper Maastrichtian Miria Formation (Carnarvon Basin), Western Australia. These units were laid down during a near-continuous marine inundation of the western margin of the Australian landmass (which followed separation from India in the Valanginian and genesis of the Indian Ocean) in the Early-Late Cretaceous. The Australian mosasaur record incorporates evidence of derived mosasaurids (mainly plioplatecarpines); however, as yet no specimen can be conclusively diagnosed to genus or species level. The fragmentary nature of the remains provides little basis for direct palaeobiogeographic comparisons. However, correlation with existing data on associated vertebrates, macroinvertebrates and microfossils suggests that the Western Australian mosasaur fauna might have been transitional in nature (particularly following palaeobiogeographic separation of the northern and southern Indian Oceans during the mid-Campanian), potentially sharing elements with both northern Tethyan and austral high-latitude regions.

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Dissertationen zum Thema "Geology Australia"

Morante, Richard. „Permian-Triassic stable isotope stratigraphy of Australia“. Phd thesis, Australia : Macquarie University, 1996. http://hdl.handle.net/1959.14/47568.

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"September, 1995"
Thesis (Ph.D.) -- Macquarie University, School of Earth Sciences, 1996.
Bibliography: leaves 171-183.
Introduction -- Australian ð¹³Corg-isotope profiles about the Permian-Triassic (P/TR) boundary -- Strontium isotope seawater curve in the late Permian of Australia -- ð¹³Cco₃ AND ð¹⁸Oco₃ seawater profiles through the Permian-Triassic of Australasia -- Paleomagnetic stratigraphy about the Permian/Triassic boundary in Australia -- Synthesis.
The Permian-Triassic boundary mass extinction is the largest in the Phanerozoic and therefore is the major event in the Phanerozoic. The mass extinction cause is problematical but studying global geochemical and geophysical signatures about the Permian-Triassic boundary can provide insights into the cause of the mass extinction. Global events about the Permian-Triassic boundary are marked by changes in: ð¹³C values of carbon ; ⁸⁷Sr/⁸⁶Sr in unaltered marine calcite ; magnetic polarity. -- This study aims to identify these features in the sedimentary record and to test the ca libration of the Australian biostratigraphical schemes to the global geological timescale. The following features are found in the Permian-Triassic sediments of Australia: a ð¹³Corg in Total Organic Carbon excursion in 12 marine and nonmarine sections from Northwest to Eastern Australia ; a ⁸⁷Sr/⁸⁶Sr minimum in a composite section mainly from the Bowen Basin ; a magnetic polarity reversal in the Cooper Basin, central Australia. The Australian sections are thus time correlated, as follows: The negative ð¹³Corg excursion indicates the Permian-Triassic boundary and occurs: 1) in Eastern and Central Australia at the change from coal measures to barren measures with red beds at the beginning of the Early Triassic coal gap; 2) in Northwest Australia about the boundary between the Hyland Bay Formation and the Mount Goodwin Formation in the Bonaparte Basin and at the boundary between the Hardman Formation and the Blina Shale in the Canning Basin. The base of the negative ð¹³Corg excursion lies at or near the base of the Protohaploxypinus microcorpuspalynological zone. The ⁸⁷Sr/⁸⁶Sr minimum determined about the Guadalupian/Ochoan stage boundary in North America is found in the Bowen Basin about the boundary between the Ingelara and Peawaddy Formations. The ð¹³Corg excursion in the Cooper Basin is near a magnetic reversal within the Permo-Triassic mixed superchron. The implications of these findings include: confirmation of the traditional placement of the Permian-Triassic boundary at the coal measures/barren measures with redbeds boundary in Eastern Australia ; the linking of the the Permian-Triassic boundary to a mass extinction of plant species on land and the beginning of the Triassic coal gap indicated by the Falcisporites Superzone base that is coincident with the negative ð¹³Corg excursion ; a mass extinction causal model that links the ⁸⁷Sr/⁸⁶Sr minimum determined about the Guadalupian/Ochoan stage boundary to a fall in sealevel that led to changing global environmental conditions. The model invokes greenhouse warming as a contributing cause of the mass extinction.
Mode of access: World Wide Web.
xii, 183 leaves ill., maps

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Bullock, Michelle. „Holocene sediments and geological history, Woolley Lake, near Beachport, South Australia /“. Adelaide : Thesis (B. Sc.(Hons)) -- University of Adelaide, Dept. of Geology and Geophysics, 1994. http://web4.library.adelaide.edu.au/theses/09SB/09sbb938.pdf.

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Shafik, Samir. „Late Cretaceous, early Tertiary calcareous nannofossils from Australia“. Title page, contents and summary only, 1989. http://hdl.handle.net/2440/19212.

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Dove, Melissa B. „The geology, petrology, geochemistry and isotope geology of the eastern St Peter Suite western Gawler Graton, South Australia /“. Title page, contents and abstract only, 1997. http://web4.library.adelaide.edu.au/theses/09SB/09sbd743.pdf.

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Thesis (B. Sc.(Hons))--University of Adelaide, Dept. of Geology and Geophysics, 1998.
National Grid Reference 1:250 000 Geological Series Sheet SI 53-2 and Sheet SI 53-6. Includes bibliographical references (6 leaves ).

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Swart, Rosemary Helen. „Environmental protection of geological monuments in South Australia /“. Title page, contents and abstract only, 1992. http://web4.library.adelaide.edu.au/theses/09ENV/09envs973.pdf.

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Williamson, Grant. „The geology and origin of manganese deposits at Pernatty Lagoon, South Australia /“. Title page, table of contents and abstract only, 1987. http://web4.library.adelaide.edu.au/theses/09SB/09sbw729.pdf.

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Millikan, Michael I. „The quaternary geology of the Pelican Lagoon area, Kangaroo Island, South Australia /“. Title page, table of contents and abstract only, 1994. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bm654.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1995.
Australian National Grid Reference Penneshaw Sheet (SI 53) 6426-I 1: 50 000. Includes bibliographical references.

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Wirtz, Peter D. „The quaternary geology of the American River area, Kangaroo Island, South Australia /“. Title page, contents and abstract only, 1994. http://web4.library.adelaide.edu.au/theses/09SB/09sbw799.pdf.

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Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1995.
Australian National Grid Reference Penneshaw Sheet (SI 53) 6246-I 1: 50 000. One col. folded map in pocket, inside back cover. Includes bibliographical references.

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Rankine, Graham M. „Gold metallogeny of Australia“. Thesis, Rhodes University, 1987. http://hdl.handle.net/10962/d1004676.

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The gold metallogeny of Australia is predominantly confined to the Archaean and Palaeozoic Provinces. The Archaean gold occurrences are predominantly hosted in ultramafic-mafic dominated greenstone belts, with less associated tofelsic-volcanic and sedimentary sequences. Most gold occurrences are confined to shear zones or faults, and adjacent discoveries of economic laterite-hosted deposits, host rocks. Recent are presently under investigation and will supply a significant proportion of production in the future. The Proterozoic gold deposits of Australia , are confined to geosyncinal sequences, commonly turbidites (eg: Telfer), with other hydrothermal deposits associated directly to granites. An important feature of the North Australian Craton deposits, is the spatial association of most deposits to granite bodies, although a genetic link has not been established conclusively. The Roxby Downs deposit in South Australia is a unique occurrence of gold in association to copper, uranium and R.E.E. This deposit is tentatively related to intraplate alkaline-magmatism, with further work necessary. The most significant recent discovery of gold mineralization in Australia is in the Drummond Basin in Queensland. This epithermal is tentatively related to mineralization within the Georgetown Inlier. The latter mineralization is Permo-Carboniferous, in a Proterozoic (and possibly Archaean) sequence of schists. It is tentatively suggested that all the gold mineralization in northern Queensland may be related to single tectonic event, a feature which requires further study . Other mineralization in the Phanerozoic includes the turbidite-hosted metamorphogenic deposits of Victoria, the rift related deposits in New South Wales and magmatic related deposits in Queensland. The gold deposits in Australia may in the future be classified in a tectonogeological framework, similiar to the layout of this dissertation, particularly once further data becomes available on recent discoveries.

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Wycherley, Helen Louise. „Origins and distribution of carbon dioxide and associated gases, Cooper Basin, Australia“. Thesis, Imperial College London, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.270974.

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Bücher zum Thema "Geology Australia"

The geology of Australia. Cambridge, UK: Cambridge University Press, 2004.

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Johnson, David. The geology of Australia. 2. Aufl. Cambridge: Cambridge University Press, 2009.

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David, Johnson. The geology of Australia. 2. Aufl. Cambridge: Cambridge University Press, 2009.

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A, Long John. Dinosaurs of Australia. Balgowlah, NSW: Reed, 1990.

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V, Preiss W., Parker A. J und Drexel J. F. 1952-, Hrsg. The geology of South Australia. Adelaide: Mines and Energy, South Australia, 1993.

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Phillips, G. Neil. Archaean gold deposits of Australia. Johannesburg: University of the Witwatersrand, 1985.

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Hocking, R. M. The Silurian Tumblagooda Sandstone, Western Australia. Perth, W.A: Geological Survey of Western Australia, 1991.

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1924-, Harrington H. J., und National Energy Research, Development and Demonstration Program (Australia), Hrsg. Permian coals of eastern Australia. Canberra: Australian Govt. Pub. Service, 1989.

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Thorne, A. M. Geology of the Ashburton Basin, Western Australia. Perth: Geology Survey of Western Australia, 1991.

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Blewett, Richard. Shaping a nation: A geology of Australia. Herausgegeben von Geoscience Australia und International Geological Congress (34th : 2012 : Brisbane, Qld.). Canberra: Geoscience Australia and ANU E-Press, 2012.

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Buchteile zum Thema "Geology Australia"

Ljung, Karin, Annemarie de Vos, Angus Cook und Philip Weinstein. „An Overview of Medical Geology Issues in Australia and Oceania“. In Medical Geology, 107–34. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-3430-4_5.

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Zhang, H. H., und B. Choi. „Foundation Design Challenges at Hunter Expressway Alliance Project in Australia“. In Springer Geology, 177–80. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-31671-5_30.

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James, Noel P., Yvonne Bone, Kirsty M. Brown und Anthony Cheshire. „Calcareous Epiphyte Production in Cool-Water Carbonate Seagrass Depositional Environments - Southern Australia“. In Perspectives in Carbonate Geology, 123–48. Chichester, West Sussex, UK: John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781444312065.ch9.

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Cooper, Barry. „Some Examples of Heritage Stones from Australia“. In Engineering Geology for Society and Territory - Volume 5, 213–18. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09048-1_41.

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Fityus, Stephen, Greg Hancock und John Gibson. „Landslides in Tertiary Basalts at Murrurundi, Australia“. In Engineering Geology for Society and Territory - Volume 2, 1061–64. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-09057-3_187.

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Lindsay, John F., und John D. Gorter. „Clastic Petroleum Reservoirs of the Late Proterozoic and Early Paleozoic Amadeus Basin, Central Australia“. In Frontiers in Sedimentary Geology, 39–74. New York, NY: Springer New York, 1993. http://dx.doi.org/10.1007/978-1-4757-0160-9_3.

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Eriksson, Kenneth A., William S. F. Kidd und Bryan Krapez. „Basin Analysis in Regionally Metamorphosed and Deformed Early Archean Terrains: Examples from Southern Africa and Western Australia“. In Frontiers in Sedimentary Geology, 371–404. New York, NY: Springer New York, 1988. http://dx.doi.org/10.1007/978-1-4612-3788-4_19.

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Lee, Serena B., und Gavin F. Birch. „Sydney Estuary, Australia: Geology, Anthropogenic Development and Hydrodynamic Processes/Attributes“. In Estuaries of the World, 17–30. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-7019-5_2.

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Baker, P., J. Woods, M. Page und F. Schlack. „The Challenges of Site Investigations, Dredging, and Land Reclamation: A Port Hedland (Western Australia) Project Perspective“. In Engineering Geology for Society and Territory - Volume 6, 299–302. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-09060-3_50.

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Lambert, I. B., J. Knutson, T. H. Donnelly und H. Etminan. „The Diverse Styles of Sediment-Hosted Copper Deposits in Australia“. In Special Publication No. 4 of the Society for Geology Applied to Mineral Deposits, 540–58. Berlin, Heidelberg: Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-642-70902-9_39.

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Konferenzberichte zum Thema "Geology Australia"

Seitzinger, Zenja. „Flow bands and microlite textures in obsidian, Minyon Falls Rhyolite, Australia“. In Proceedings of the Keck Geology Consortium. Keck Geology Consortium, 2020. http://dx.doi.org/10.18277/akrsg.2020.33.12.

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Campo, Chloe. „Pre-eruptive temperatures and eruption dynamics of rhyolite lava, Nimbin rhyolite, eastern Australia“. In Proceedings of the Keck Geology Consortium. Keck Geology Consortium, 2020. http://dx.doi.org/10.18277/akrsg.2020.33.10.

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Seggie*, Robert. „Dinoturbation of the Broome Sandstone — Implications for Petroleum Geology“. In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2188421.

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Dykstra, Brooke. „Microlite orientations and strain localization within the basal shear zone of a large rhyolitic lava, Minyon Falls, Australia“. In Proceedings of the Keck Geology Consortium. Keck Geology Consortium, 2020. http://dx.doi.org/10.18277/akrsg.2020.33.11.

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Eshmawi, Yosuf. „The Geology and 3D Modelling of the Cliff Head Oil Field, Australia“. In SPE Middle East Oil and Gas Show and Conference. Society of Petroleum Engineers, 2019. http://dx.doi.org/10.2118/194954-ms.

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Totterdell*, Jennifer, Lisa Hall, Takehiko Hashimoto und Kathryn Owen. „The Petroleum Potential of Australian Offshore Frontier Basins: Geology, Data, Opportunities and Challenges“. In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2210758.

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Telesford, Arthur Linus, Sharon Kah Heng Cheong, Timothy Brett Cotton und Simon T. Chipperfield. „Geology Drives Technology - Application of Coil Tubing Underbalanced Drilling in the Cooper Basin, Australia“. In International Petroleum Technology Conference. International Petroleum Technology Conference, 2008. http://dx.doi.org/10.2523/iptc-12439-ms.

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Telesford, A. L., S. Cheong, T. Cotton und S. Chipperfield. „‘Geology Drives Technology’—Application of Coil Tubing Underbalanced Drilling in the Cooper Basin, Australia“. In IPTC 2008: International Petroleum Technology Conference. European Association of Geoscientists & Engineers, 2008. http://dx.doi.org/10.3997/2214-4609-pdb.148.iptc12439.

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Sapiie*, Benyamin, Harya Danio, Ariesty Asikin und Awali Priyono. „Geology and Geomechanics Evaluation of CCS Pilot Project in The Gundih Field, East Java Basin, Indonesia“. In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2210557.

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Kivior, Irena, Stephen Markham und Leslie Mellon. „Mapping Sub-Surface Geology From Magnetic Data in the Hides Area, Western Papuan Fold Belt, Papua New Guinea“. In International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2210793.

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Berichte der Organisationen zum Thema "Geology Australia"

Jackson, L. E. Surficial geology, Australia Mountain, Yukon Territory. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2005. http://dx.doi.org/10.4095/220181.

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Picard, Kim, Scott L. Nichol, Riko Hashimoto, Andrew Carroll, George Bernadel, Leonie Jones, Justy Siwabessy et al. Seabed environments and shallow geology of the Leveque Shelf, Browse Basin, Western Australia. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.010.

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Stewart, A. J. Notes on North Australia Craton solid geology maps: Northern Territory-Queensland, 2015-20. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.012.

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Nicholas, W. A., A. G. Carroll, L. Radke, M. Tran, F. J. F. Howard, R. Przeslawski, J. Chen, P. J. W. Siwabessy, und S. L. Nichol. Seabed Environments and Shallow Geology of the Leveque Shelf, Browse Basin, Western Australia: GA0340 - Interpretative report. Geoscience Australia, 2016. http://dx.doi.org/10.11636/record.2016.018.

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Caritat, P. de, und U. Troitzsch. Towards a regolith mineralogy map of the Australian continent: a feasibility study in the Darling-Curnamona-Delamerian region. Geoscience Australia, 2021. http://dx.doi.org/10.11636/record.2021.035.

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Annotation:

Bulk quantitative mineralogy of regolith is a useful indicator of lithological precursor (protolith), degree of weathering, and soil properties affecting various potential landuse decisions. To date, no national-scale maps of regolith mineralogy are available in Australia. Catchment outlet sediments collected over 80% of the continent as part of the National Geochemical Survey of Australia (NGSA) afford a unique opportunity to rapidly and cost-effectively determine regolith mineralogy using the archived sample material. This report releases mineralogical data and metadata obtained as part of a feasibility study in a selected pilot area for such a national regolith mineralogy database and atlas. The area chosen for this study is within the Darling-Curnamona-Delamerian (DCD) region of southeastern Australia. The DCD region was selected as a ‘deep-dive’ data acquisition and analysis by the Exploration for the Future (2020-2024) federal government initiative managed at Geoscience Australia. One hundred NGSA sites from the DCD region were prepared for X-Ray Diffraction (XRD) analysis, which consisted of qualitative mineral identification of the bulk samples (i.e., ‘major’ minerals), qualitative clay mineral identification of the <2 µm grain-size fraction, and quantitative analysis of both ‘major’ and clay minerals of the bulk sample. The identified mineral phases were quartz, plagioclase, K-feldspar, calcite, dolomite, gypsum, halite, hematite, goethite, rutile, zeolite, amphibole, talc, kaolinite, illite (including muscovite and biotite), palygorskite (including interstratified illite-smectite and vermiculite), smectite (including interstratified illite-smectite), vermiculite, and chlorite. Poorly diffracting material (PDM) was also quantified and reported as ‘amorphous’. Mineral identification relied on the EVA® software, whilst quantification was performed using Siroquant®. Resulting mineral abundances are reported with a Chi-squared goodness-of-fit between the actual diffractogram and a modelled diffractogram for each sample, as well as an estimated standard error (esd) measurement of uncertainty for each mineral phase quantified. Sensitivity down to 0.1 wt% (weight percent) was achieved, with any mineral detection below that threshold reported as ‘trace’. Although detailed interpretation of the mineralogical data is outside the remit of the present data release, preliminary observations of mineral abundance patterns suggest a strong link to geology, including proximity to fresh bedrock, weathering during sediment transport, and robust relationships between mineralogy and geochemistry. The mineralogical data generated by this study are presented in Appendix A of this report and are downloadable as a .csv file. Mineral abundance or presence/absence maps are shown in Appendices B and C to document regional mineralogical patterns.

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Stewart, A. J., S. F. Liu, M. A. Bonnardot, L. M. Highet, M. Woods, C. Brown, K. Czarnota und K. Connors. Seamless chronostratigraphic solid geology of the North Australian Craton. Geoscience Australia, 2020. http://dx.doi.org/10.11636/134486.

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Totterdell, Jennifer, Lisa Hall, Riko Hashimoto, Kathryn Owen und Marita Bradshaw. Petroleum geology inventory of Australia’s offshore frontier basins. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.009.

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Geologic investigations of the 1986 Marryat Creek, Australia, earthquake; implications for paleoseismicity in stable continental regions. US Geological Survey, 1993. http://dx.doi.org/10.3133/b2032b.

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Geologic map of the MTM -85280 quadrangle, Planum Australe region of Mars. US Geological Survey, 1998. http://dx.doi.org/10.3133/i2595.

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Geologic Map of the MTM-85000 Quadrangle, Planum Australe Region of Mars. US Geological Survey, 2001. http://dx.doi.org/10.3133/i2686.

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