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Articoli di riviste sul tema "Geology Australia"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 28 luglio 2024

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1

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, no. 6 (June 6, 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)

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2

Plumb, K. A. "Proterozoic geology of Australia and palaeomagnetism." Exploration Geophysics 24, no. 2 (June 1993): 213–18. http://dx.doi.org/10.1071/eg993213.

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3

Groves, David I., Mark E. Barley, and Julie M. Shepherd. "Geology and Mineralisation of Western Australia." Exploration Geophysics 25, no. 3 (September 1994): 163. http://dx.doi.org/10.1071/eg994163.

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4

Nott, Jonathan F. "The urban geology of Darwin, Australia." Quaternary International 103, no. 1 (January 2003): 83–90. http://dx.doi.org/10.1016/s1040-6182(02)00143-x.

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5

Cook, Robert B. "Ataeamite: Moonta Mine, South Australia, Australia." Rocks & Minerals 81, no. 5 (January 2006): 374–78. http://dx.doi.org/10.3200/rmin.81.5.374-378.

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6

Jworchan, Indra, Tony O' Brien, Emged Rizkalla, and Paul Gorman. "Engineering geology of Waterside Green, Sydney, Australia." Journal of Nepal Geological Society 34 (October 9, 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 investi

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7

Nott, Jonathan F. "The urban geology of Cairns, Queensland, Australia." Quaternary International 103, no. 1 (January 2003): 75–82. http://dx.doi.org/10.1016/s1040-6182(02)00142-8.

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8

Groves, David I., Mark E. Barley, and Julie M. Shepherd. "OVERVIEWS: Geology and mineralisation of Western Australia." ASEG Extended Abstracts 1994, no. 1 (December 1994): 1–28. http://dx.doi.org/10.1071/asegspec07_02.

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9

McNally, G. H. "Some issues in environmental geology in Australia." Australian Journal of Earth Sciences 47, no. 1 (February 2000): 1. http://dx.doi.org/10.1046/j.1440-0952.2000.00767.x.

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10

Kear, B. P., J. A. Long, and J. E. Martin. "A review of Australian mosasaur occurrences." Netherlands Journal of Geosciences 84, no. 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 mo

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11

Ripperdan, R. L., M. Magaritz, and J. L. Kirschvink. "Carbon isotope and magnetic polarity evidence for non-depositional events within the Cambrian-Ordovician Boundary section near Dayangcha, Jilin Province, China." Geological Magazine 130, no. 4 (July 1993): 443–52. http://dx.doi.org/10.1017/s0016756800020525.

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AbstractCarbon isotope and magnetic polarity stratigraphic results from the Cambrian-Ordovician Boundary section at Xiaoyangqiao, near Dayangcha, Jilin Province, China, in comparison to a contemporaneous section at Black Mountain, Australia, indicate strata equivalent to major portions of the Australian sequence are either absent or are restricted to highly condensed intervals. These intervals are correlative with regressive sea level events identified in Australia and western North America, suggesting regional or eustatic sea level changes strongly influenced deposition of the Xiaoyangqiao se

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12

Phillips, Ryan D., Gary Backhouse, Andrew P. Brown, and Stephen D. Hopper. "Biogeography of Caladenia (Orchidaceae), with special reference to the South-west Australian Floristic Region." Australian Journal of Botany 57, no. 4 (2009): 259. http://dx.doi.org/10.1071/bt08157.

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Caladenia contains 376 species and subspecies, of which almost all are endemic to temperate and southern semiarid Australia. Eleven species occur in New Zealand, 10 of which are endemic, and one species is widely distributed in eastern Australia and the western Pacific. Only three species occur in both south-western and south-eastern Australia. At subgeneric level, Drakonorchis is endemic to the South-west Australian Floristic Region (SWAFR), Stegostyla to eastern Australia and New Zealand, whereas three subgenera, Calonema, Phlebochilus and Elevatae occur on both sides of the Nullarbor Plain.

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13

Robin, Libby, Steve Morton, and Mike Smith. "Writing a History of Scientific Endeavour in Australia’s Deserts." Historical Records of Australian Science 25, no. 2 (2014): 143. http://dx.doi.org/10.1071/hr14011.

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This special issue of Historical Records of Australian Science explores some of the sciences that have contributed to our understanding of inland Australia, country variously known as desert, the arid zone, drylands and the outback. The sciences that have concentrated on deserts include ecology, geomorphology, hydrology, rangeland management, geography, surveying, meteorology and geology, plus many others. In recognition that desert science has surged ahead in the past few decades, we have invited contributors who describe various different desert initiatives. We use these case studies to open

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14

Cawood, P. A., E. C. Leitch, R. E. Merle, and A. A. Nemchin. "Orogenesis without collision: Stabilizing the Terra Australis accretionary orogen, eastern Australia." Geological Society of America Bulletin 123, no. 11-12 (June 24, 2011): 2240–55. http://dx.doi.org/10.1130/b30415.1.

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15

Chessman, Bruce C., Nina Bate, Peter A. Gell, and Peter Newall. "A diatom species index for bioassessment of Australian rivers." Marine and Freshwater Research 58, no. 6 (2007): 542. http://dx.doi.org/10.1071/mf06220.

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The Diatom Index for Australian Rivers (DIAR), originally developed at the genus level, was reformulated at the species level with data from diatom sampling of rivers in the Australian Capital Territory, New South Wales, Queensland, South Australia and Victoria. The resulting Diatom Species Index for Australian Rivers (DSIAR) was significantly correlated with the ARCE (Assessment of River Condition, Environment) index developed in the Australian National Land and Water Resources Audit (NLWRA), and with nine of the ARCE’s constituent indices and sub-indices, across 395 river reaches in south-ea

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16

Davis, Larry. "My Geological Connection between Minnesota and Western Australia." Compass: Earth Science Journal of Sigma Gamma Epsilon 85, no. 1 (July 30, 2013): 1–9. http://dx.doi.org/10.62879/c95401030.

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Even though the flora and fauna of Minnesota and Western Australia are vastly different, there are some similarities in the geology. This essay illustrates the author’s geological connection between Minnesota, USA and Western Australia.

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17

Mcnamara, Kenneth, and Frances Dodds. "The Early History of Palaeontology in Western Australia: 1791-1899." Earth Sciences History 5, no. 1 (January 1, 1986): 24–38. http://dx.doi.org/10.17704/eshi.5.1.t85384660311h176.

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The exploration of the coast of Western Australia by English and French explorers in the late eighteenth and early nineteenth centuries led to the first recorded discoveries of fossiliferous rocks in Western Australia. The first forty years of exploration and discovery of fossil sites in the State was restricted entirely to the coast of the Continent. Following the establishment of permanent settlements in the 1820s the first of the inland fossil localities were located in the 1830s, north of Albany, and north of Perth. As new land was surveyed; particularly north of Perth, principally by the

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18

Newton, Warwick, Sue Daly, Stuart Robertson, Wolfgang Preiss, Colin conor, and Andrew Burtt. "Overview of geology and mineralisation in South Australia." ASEG Extended Abstracts 2003, no. 3 (December 2003): 1–18. http://dx.doi.org/10.1071/asegspec12_01.

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19

Howard, Kieren T., and Peter W. Haines. "The geology of Darwin Crater, western Tasmania, Australia." Earth and Planetary Science Letters 260, no. 1-2 (August 2007): 328–39. http://dx.doi.org/10.1016/j.epsl.2007.06.007.

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20

Salmachi, Alireza, Mojtaba Rajabi, Carmine Wainman, Steven Mackie, Peter McCabe, Bronwyn Camac, and Christopher Clarkson. "History, Geology, In Situ Stress Pattern, Gas Content and Permeability of Coal Seam Gas Basins in Australia: A Review." Energies 14, no. 9 (May 5, 2021): 2651. http://dx.doi.org/10.3390/en14092651.

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Coal seam gas (CSG), also known as coalbed methane (CBM), is an important source of gas supply to the liquefied natural gas (LNG) exporting facilities in eastern Australia and to the Australian domestic market. In late 2018, Australia became the largest exporter of LNG in the world. 29% of the country’s LNG nameplate capacity is in three east coast facilities that are supplied primarily by coal seam gas. Six geological basins including Bowen, Sydney, Gunnedah, Surat, Cooper and Gloucester host the majority of CSG resources in Australia. The Bowen and Surat basins contain an estimated 40Tcf of

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21

Carr, Lidena, Russell Korsch, and Tehani Palu. "Australia's onshore basin inventory: volume I." APPEA Journal 56, no. 2 (2016): 591. http://dx.doi.org/10.1071/aj15097.

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Following the publication of Geoscience Australia Record 2014/09: Petroleum geology inventory of Australia’s offshore frontier basins by Totterdell et al (2014), the onshore petroleum section of Geoscience Australia embarked on a similar project for the onshore Australian basins. Volume I of this publication series contains inventories of the McArthur, South Nicholson, Georgina, Amadeus, Warburton, Wiso, Galilee, and Cooper basins. A comprehensive review of the geology, petroleum systems, exploration status, and data coverage for these eight Australian onshore basins was conducted, based on th

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22

Graham, Lan T., and Ross E. Pogson. "The Albert Chapman Mineral Collection: Australian Museum, Sydney, New South Wales, Australia." Rocks & Minerals 82, no. 1 (January 2007): 29–39. http://dx.doi.org/10.3200/rmin.82.1.29-39.

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23

Shragge, Jeffrey, David Lumley, Julien Bourget, Toby Potter, Taka Miyoshi, Ben Witten, Jeremie Giraud, et al. "The Western Australia Modeling project — Part 2: Seismic validation." Interpretation 7, no. 4 (November 1, 2019): T793—T807. http://dx.doi.org/10.1190/int-2018-0218.1.

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Large-scale 3D modeling of realistic earth models is being increasingly undertaken in industry and academia. These models have proven useful for various activities such as geologic scenario testing through seismic finite-difference (FD) modeling, investigating new acquisition geometries, and validating novel seismic imaging, inversion, and interpretation methods. We have evaluated the results of the Western Australia (WA) Modeling (WAMo) project, involving the development of a large-scale 3D geomodel representative of geology of the Carnarvon Basin, located offshore of WA’s North West Shelf (N

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24

Burrett, Clive, and Ronald Berry. "Proterozoic Australia–Western United States (AUSWUS) fit between Laurentia and Australia." Geology 28, no. 2 (2000): 103. http://dx.doi.org/10.1130/0091-7613(2000)28<103:pausaf>2.0.co;2.

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25

Klootwijk, Chris. "Middle–Late Paleozoic Australia–Asia convergence and tectonic extrusion of Australia." Gondwana Research 24, no. 1 (July 2013): 5–54. http://dx.doi.org/10.1016/j.gr.2012.10.007.

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26

J. Hobbs, Richard. "The wheatbelt of Western Australia." Pacific Conservation Biology 9, no. 1 (2003): 9. http://dx.doi.org/10.1071/pc030009.

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DEVELOPMENT for broadscale wheat and sheep farming in Western Australia has produced a seemingly uniform landscape over much of the southwest of Western Australia. However, this area, commonly called the wheatbelt (Fig. 1), consists of at least four of the biogeographic regions designated on the basis of physical and biological measures (such as climate, geology, landform landuse, flora and fauna) in the Interim Biogeographic Regionalization of Australia (Thackway and Cresswell 1994). The four Interim Biogeographic Regionalization of Australia regions making up the wheatbelt are the Geraldton

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27

Bell, Phil R., Russell D. C. Bicknell, and Elizabeth T. Smith. "Crayfish bio-gastroliths from eastern Australia and the middle Cretaceous distribution of Parastacidae." Geological Magazine 157, no. 7 (October 30, 2019): 1023–30. http://dx.doi.org/10.1017/s0016756819001092.

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AbstractFossil crayfish are typically rare, worldwide. In Australia, the strictly Southern Hemisphere clade Parastacidae, while ubiquitous in modern freshwater systems, is known only from sparse fossil occurrences from the Aptian–Albian of Victoria. We expand this record to the Cenomanian of northern New South Wales, where opalized bio-gastroliths (temporary calcium storage bodies found in the foregut of pre-moult crayfish) form a significant proportion of the fauna of the Griman Creek Formation. Crayfish bio-gastroliths are exceedingly rare in the fossil record but here form a remarkable supp

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28

Dudicourt, Jean-Christophe, Didier Neraudeau, Philippe Nicolleau, Luc Ceulemans, and Frédéric Boutin. "An outstanding fauna of marsupiate echinoids in the Pliocene of Vendée (western France)." Bulletin de la Société Géologique de France 176, no. 6 (November 1, 2005): 545–57. http://dx.doi.org/10.2113/176.6.545.

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Abstract New investigations in the Pliocene deposits of Challans (Vendée) have allowed to collect more than 3000 marsupiate echinoids, remarkably preserved. So, apical systems, especially the marsupium of the breeding temnopleurids T. (V.) bigoti and C. bardini, have been described and figured for the first time with complete specimens. Two new marsupiate species have been described: Arbacina hugueti nov. sp., third marsupiate species of the genus Arbacina to be known in the Neogene of western France after A. emmae NÉRAUDEAU, 2003 from the Messinian of Brittany and A. pareyni ROMAN, 1983 fro

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29

Gibson, G. M., and D. C. Champion. "Antipodean fugitive terranes in southern Laurentia: How Proterozoic Australia built the American West." Lithosphere 11, no. 4 (June 10, 2019): 551–59. http://dx.doi.org/10.1130/l1072.1.

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Abstract Paleoproterozoic arc and backarc assemblages accreted to the south Laurentian margin between 1800 Ma and 1600 Ma, and previously thought to be indigenous to North America, more likely represent fragments of a dismembered marginal sea developed outboard of the formerly opposing Australian-Antarctic plate. Fugitive elements of this arc-backarc system in North America share a common geological record with their left-behind Australia-Antarctic counterparts, including discrete peaks in tectonic and/or magmatic activity at 1780 Ma, 1760 Ma, 1740 Ma, 1710–1705 Ma, 1690–1670 Ma, 1650 Ma, and

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30

V.A., Shuper. "Geography of Australia And Oceania: «From Geology To Ideology»." MGIMO Review of International Relations 6, no. 63 (December 1, 2018): 317–24. http://dx.doi.org/10.24833/2071-8160-2018-6-63-317-324.

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31

Wilde, A. R., and V. J. Wall. "Geology of the Nabarlek uranium deposit, Northern Territory, Australia." Economic Geology 82, no. 5 (August 1, 1987): 1152–68. http://dx.doi.org/10.2113/gsecongeo.82.5.1152.

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32

Willey, E. C. "Urban geology of the Toowoomba conurbation, SE Queensland, Australia." Quaternary International 103, no. 1 (January 2003): 57–74. http://dx.doi.org/10.1016/s1040-6182(02)00141-6.

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33

Catto, Norm, and Peter Bobrowsky. "Urban and Quaternary geology, New Zealand and eastern Australia." Quaternary International 103, no. 1 (January 2003): 1–2. http://dx.doi.org/10.1016/s1040-6182(02)00177-5.

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34

Walter, Malcolm. "The geology of South Australia, volume 1. The Precambrian." Precambrian Research 78, no. 4 (June 1996): 298–99. http://dx.doi.org/10.1016/0301-9268(95)00060-7.

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35

Laznicka, P. "Geology and economics of platinum-group metals in Australia." Ore Geology Reviews 5, no. 3 (February 1990): 247. http://dx.doi.org/10.1016/0169-1368(90)90013-d.

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36

Gatehouse, Colin G. "The geology of the Warburton Basin in South Australia." Australian Journal of Earth Sciences 33, no. 2 (June 1986): 161–80. http://dx.doi.org/10.1080/08120098608729357.

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37

Percival, I. G., and P. M. Cooney. "PETROLEUM GEOLOGY OF THE MERLINLEIGH SUB-BASIN, WESTERN AUSTRALIA." APPEA Journal 25, no. 1 (1985): 190. http://dx.doi.org/10.1071/aj84017.

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Esso's recent drilling program in the Merlinleigh Sub-basin, onshore Carnarvon Basin, represents the culmination of the first phase of concerted exploration activity in the area since the WAPET era of the 1960s. The region is unusual among Australian petroleum provinces in having excellent exposures of reservoir, source and seal rocks of Palaeozoic age. While both Esso wells (Burna 1 and Gascoyne 1) failed to encounter hydrocarbons in the primary Wooramel Group play, encouraging potential still exists. The reservoir in the Wooramel Group play is the Early Permian Moogooloo Sandstone, a fluviod

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38

Osborne, D. G., and E. A. Howell. "THE GEOLOGY OF THE HARRIET OILFIELD, OFFSHORE WESTERN AUSTRALIA." APPEA Journal 27, no. 1 (1987): 152. http://dx.doi.org/10.1071/aj86014.

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The Harriet Oilfield, discovered in November 1988, is situated within offshore permit WA-192-P in the Barrow Sub-basin. Following the Harriet 1 discovery well, detailed seismic surveys were recorded and a further ten wells were drilled on the structure between 1988 and 1985. Nine of the wells were completed as producers and one was plugged and abandoned as a dry hole.The oil accumulation occurs in a low relief, fault-dependent closure on the upthrown side of the Lowendal Fault. The trap is mainly structurally controlled but stratigraphic barriers are believed to be locally present, based on di

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39

COOPER, BARRY J., and JAMES B. JAGO. "ROBERT BEDFORD (1874–1951), THE KYANCUTTA MUSEUM, AND A UNIQUE CONTRIBUTION TO INTERNATIONAL GEOLOGY." Earth Sciences History 37, no. 2 (January 1, 2018): 416–43. http://dx.doi.org/10.17704/1944-6178-37.2.416.

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Robert Bedford (1874–1951), based in the isolated community of Kyancutta in South Australia, was a unique contributor to world geology, specifically in the field of meteorites and fossil archaeocyatha. Born Robert Arthur Buddicom in Shropshire, UK, he was an Oxford graduate who worked as a scientist in Freiberg, Naples, Birmingham and Shrewsbury as well as with the Natural History Museum, Kensington and the Plymouth Museum in the United Kingdom. He was a Fellow of the Geological Society of London, 1899–1910. In 1915, Buddicom changed his surname to Bedford and relocated to South Australia. Dur

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40

Karanth, R. V. "Gemstones of Western Australia." Journal of the Geological Society of India 82, no. 3 (September 2013): 299–300. http://dx.doi.org/10.1007/s12594-013-0154-z.

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Cook, Robert B. "Crocoite: Dundas, Tasmania, Australia." Rocks & Minerals 82, no. 1 (January 2007): 50–54. http://dx.doi.org/10.3200/rmin.82.1.50-54.

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42

Downes, Peter J., and Alex W. R. Bevan. "Diamonds in Western Australia." Rocks & Minerals 82, no. 1 (January 2007): 66–73. http://dx.doi.org/10.3200/rmin.82.1.66-73.

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43

Thompson, Timothy, Jared Priddle, and Jurij Karlovsek. "The Queensland geotechnical database." Australian Geomechanics Journal 59, no. 1 (March 1, 2024): 93–102. http://dx.doi.org/10.56295/agj5915.

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The Queensland Geotechnical Database (QGD; qgd.org.au) was launched in October 2017 with the aim of consolidating primarily tax and toll-payer subsidised geotechnical investigation logs into an open platform. The QGD was influenced by public geotechnical databases in the United Kingdom and New Zealand, and the work of Robert Leggett in Canada as summarised in ‘Cities and Geology’ (1973). As of October 2023, the QGD includes over 3100 geotechnical investigation logs authored by over 10 public and private entities, dating back to 1966. It also includes national geological mapping and links to ov

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44

WARREN, A. A., R. DAMIANI, and A. M. YATES. "The South African stereospondyl Lydekkerina huxleyi (Tetrapoda, Temnospondyli) from the Lower Triassic of Australia." Geological Magazine 143, no. 6 (September 4, 2006): 877–86. http://dx.doi.org/10.1017/s0016756806002524.

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The first tetrapod fossil from the Rewan Formation of the Galilee Basin, central Queensland, Australia, is identified as Lydekkerina huxleyi, a stereospondyl found elsewhere only in the Lystrosaurus Assemblage Zone of South Africa. Apomorphies shared with L. huxleyi are: anterior palatal vacuity with anterodorsal projections from its posterior margin; ventral surface of skull roof with series of thickened ridges (condition unknown in other lydekkerinids); and vomerine shagreen present (possible autapomorphic reversal). Restudy of the only other Australian lydekkerinid, Chomatobatrachus halei,

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TOPPER, TIMOTHY P., GLENN A. BROCK, CHRISTIAN B. SKOVSTED, and JOHN R. PATERSON. "Palaeoscolecid scleritome fragments with Hadimopanella plates from the early Cambrian of South Australia." Geological Magazine 147, no. 1 (June 16, 2009): 86–97. http://dx.doi.org/10.1017/s0016756809990082.

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AbstractPhosphatized articulated palaeoscolecid scleritome fragments with attached Hadimopanella Gedik, 1977 plates are described from the lower Cambrian Mernmerna Formation of South Australia. Hadimopanella is principally known from single, isolated, button-shaped, phosphatic sclerites. The new articulated material from South Australia reveals for the first time the configuration of plates referable to Hadimopanella within the scleritome. The scleritome fragments represent the main trunk sections of the cuticle with anterior and posterior terminations lacking. Each annulus on the trunk is orn

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46

Dawes, P. R., and C. P. Swager. "Organisational bonus through staff rejuvenation: Greenland-Australia exchange." Bulletin Grønlands Geologiske Undersøgelse 172 (January 1, 1996): 9–14. http://dx.doi.org/10.34194/bullggu.v172.6736.

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This paper deals with an example of a short-term staff exchange (9 months) between Copenhagen and Perth, and the benefits gained, both on organisational and individual levels. The theme of this paper is mainly concerned with Precambrian geology, although the general premises discussed may equally apply to other geological fields.

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Corbett, David. "The Foundations of South Australian Geology : 1802-1860." Earth Sciences History 6, no. 2 (January 1, 1987): 146–58. http://dx.doi.org/10.17704/eshi.6.2.146u45l482734411.

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Abstract (sommario):

The Colony of South Australia was founded at a time when the science of geology was developing rapidly and increasing in popularity among all levels of society. Adelaide, the foundation city, had good reason to foster its 'sense of difference' from the other colonies in Australia, being largely isolated from them, but also, and more significantly, because it had been established by free settlers. Among these was a group of well-educated men concerned with geological matters - partly from necessity and the need to locate useful natural resources but equally, imbued with a well-developed sense o

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48

Hashimoto, Takehiko, Karen Higgins, Nadege Rollet, Vaughan Stagpoole, Peter Petkovic, Jim Colwell, Ron Hackney, Graham Logan, R. Funnell, and George Bernardel. "Geology and prospectivity of the Capel and Faust basins in the deepwater Tasman Sea region." APPEA Journal 51, no. 2 (2011): 702. http://dx.doi.org/10.1071/aj10082.

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Geoscience Australia recently completed a petroleum prospectivity assessment of the Capel and Faust basins as part of the Australian government's energy security program. This pre-competitive study was carried out in collaboration with GNS Science and the government of New Caledonian, and was based on seismic, potential field, multibeam bathymetry and sample data acquired during marine surveys in 2006–7. The Capel and Faust basins are located in the Tasman Sea region, which contains a number of deepwater basins. There is little information about their geology. The Geoscience Australia study co

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Ortega-Gutiérrez, Fernando, and J. Duncan Keppie. "Proterozoic Australia–Western United States (AUSWUS) fit between Laurentia and Australia: Comment and Reply." Geology 28, no. 9 (2000): 863. http://dx.doi.org/10.1130/0091-7613(2000)28<863:pausaf>2.0.co;2.

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50

Burrett, Clive, and Ronald Berry. "Proterozoic Australia–Western United States (AUSWUS) fit between Laurentia and Australia: Comment and Reply." Geology 28, no. 9 (2000): 863. http://dx.doi.org/10.1130/0091-7613(2000)28<864:pausaf>2.0.co;2.

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