Готові списки джерел за темами / Proterozoic Australia

Добірка наукової літератури з теми "Proterozoic Australia"

Автор: Grafiati
Опубліковано: 10 грудня 2022
Оновлено: 28 січня 2023

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Статті в журналах з теми "Proterozoic Australia"

1

Myers, John S., Russell D. Shaw, and Ian M. Tyler. "Tectonic evolution of Proterozoic Australia." Tectonics 15, no. 6 (December 1996): 1431–46. http://dx.doi.org/10.1029/96tc02356.

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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

McLaren, Sandra, Mike Sandiford, and Roger Powell. "Contrasting styles of Proterozoic crustal evolution: A hot-plate tectonic model for Australian terranes." Geology 33, no. 8 (August 1, 2005): 673–76. http://dx.doi.org/10.1130/g21544ar.1.

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Abstract Proterozoic terranes in Australia record complex tectonic histories in the interval 1900– 1400 Ma that have previously been interpreted by means of simple intracratonic or plate-tectonic models. However, these models do not fully account for (1) repeated tectonic reactivation (both orogenesis and rifting), (2) mainly high-temperature–low-pressure metamorphism, (3) rifting and sag creating thick sedimentary basins, (4) the nature and timing of voluminous felsic magmatism, (5) relatively large aspect ratio orogenic belts, and (6) a general paucity of diagnostic plate-boundary features. A key to understanding these histories is the observation that Australian Proterozoic terranes are characterized by an extraordinary, but heterogeneous, enrichment of the heat-producing elements. This enrichment must contribute to long-term lithospheric weakening, and thus we advocate a hybrid lithospheric evolution model with two tectonic switches: plate-boundary–derived stresses and heat-producing-element–related lithospheric weakening. The Australian Proterozoic crustal growth record is therefore a function of the magnitude of these stresses, the way in which the heat-producing elements are distributed, and how both of these change with time.
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4

Cawood, P. A., and R. J. Korsch. "Assembling Australia: Proterozoic building of a continent." Precambrian Research 166, no. 1-4 (October 2008): 1–35. http://dx.doi.org/10.1016/j.precamres.2008.08.006.

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5

Townson, W. G. "THE SUBSURFACE GEOLOGY OF THE WESTERN OFFICER BASIN — RESULTS OF SHELL'S 1980-1984 PETROLEUM EXPLORATION CAMPAIGN." APPEA Journal 25, no. 1 (1985): 34. http://dx.doi.org/10.1071/aj84003.

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The Officer Basin described in this paper includes four Proterozoic to Lower Palaeozoic sub-basins (Gibson, Yowalga, Lennis, Waigen) which extend in a northwest to southeast belt across 200 000 sq. km of central Western Australia. These sub-basins are bounded by Archaean to Proterozoic basement blocks and are almost entirely concealed by a veneer of Permian and Cretaceous sediments. Depth to magnetic basement locally exceeds eight kilometres.Until recently, information on the sub-surface geology was limited to shallow levels, based on the results of a petroleum exploration campaign in the 1960s and the work of State and Federal Geological Surveys. In 1980, the Shell Company of Australia was awarded three permits (46 200 sq. km) covering the Yowalga and Lennis Sub-basins. The results of 4700 km of seismic data and three deep wildcat wells, combined with gravity, aeromagnetic, Landsat, outcrop and corehole information, has led to a better understanding of the regional subsurface geology.The Lennis Sub-basin appears to contain Lower to Middle Proterozoic sediments, whereas the Yowalga Sub- basin is primarily an Upper Proterozoic to Lower Cambrian sequence which comprises a basal clastic section, a middle carbonate and evaporite sequence and an upper clastic section. Widespread Middle Cambrian basalts cap the Upper Proterozoic to Lower Cambrian prospective sequence. Late Proterozoic uplift resulted in salt- assisted gravity tectonics leading to complex structural styles, especially in the basin axis.Despite oil shows, organic matter in the oil and gas generation windows and reservoir-quality sandstones with interbedded shales, no convincing source rocks or hydrocarbon accumulations have yet been located. The area remains, however, one of the least explored basins in Australia.
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Burrett, Clive, and Ronald Berry. "Proterozoic Australia–Western United States (AUSWUS) fit between Laurentia and Australia." Geology 28, no. 2 (February 2000): 103–6. http://dx.doi.org/10.1130/0091-7613(2000)028<0103:pawusa>2.3.co;2.

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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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Uysal, I. Tonguç, Claudio Delle Piane, Andrew James Todd, and Horst Zwingmann. "Precambrian faulting episodes and insights into the tectonothermal history of north Australia: microstructural evidence and K–Ar, <sup>40</sup>Ar–<sup>39</sup>Ar, and Rb–Sr dating of syntectonic illite from the intracratonic Millungera Basin." Solid Earth 11, no. 5 (September 4, 2020): 1653–79. http://dx.doi.org/10.5194/se-11-1653-2020.

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Abstract. Australian terranes concealed beneath Mesozoic cover record complex Precambrian tectonic histories involving a successive development of several Proterozoic to Palaeozoic orogenic systems. This study presents an integrated approach combining K–Ar, 40Ar–39Ar, and Rb–Sr geochronologies of Precambrian authigenic illites from the recently discovered Millungera Basin in north-central Australia. Brittle deformation and repeated fault activity are evident from the sampled cores and their microstructures, probably associated with the large-scale faults inferred from interpretations of seismic surveys. Rb–Sr isochron, 40Ar–39Ar total gas, and K–Ar ages are largely consistent in indicating late Mesoproterozoic and early Proterozoic episodes (∼1115±26, ∼ 1070±25, ∼1040±24, ∼1000±23, and ∼905±21 Ma) of active tectonics in north-central Australia. K–Ar results show that illites from fault gouges and authigenic matrix illites in undeformed adjacent sandstones precipitated contemporaneously, indicating that advection of tectonically mobilized fluids extended into the undeformed wall rocks above or below the fracture and shear (fault gouge) zones. Isotopic age data clearly indicate a Mesoproterozoic minimum age for the Millungera Basin and thus previously unrecorded late Mesoproterozoic–early Neoproterozoic tectonic events in north-central Australia. This study provides insight into the enigmatic time–space distribution of Precambrian tectonic zones in central Australia, which are responsible for the formation of a number of sedimentary basins with significant energy and mineral resources.
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Wyborn, L. A. I., D. Wyborn, R. G. Warren, and B. J. Drummond. "Proterozoic granite types in Australia: implications for lower crust composition, structure and evolution." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 83, no. 1-2 (1992): 201–9. http://dx.doi.org/10.1017/s0263593300007896.

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ABSTRACTGranites and their associated comagmatic felsic volcanic rocks occur in most Proterozoic provinces of Australia. Using multi-element, primordial-mantle-normalised abundance diagrams and various petrological characteristics, Australian Proterozoic granites can be subdivided into five groups: (i) I-type, Sr-depleted, Y-undepleted, restite-dominated, (ii) I- type, Sr-depleted, Y-undepleted, fractionated, low in incompatible elements, (iii) I-type Sr-depleted, Y-undepleted, enriched in incompatible elements (anorogenic granites), (iv) I-type, Sr-undepleted, Y-depleted, (v) S-type, Sr-depleted, Y-undepleted. The four Sr-depleted groups dominate, and group (iv) is of very limited extent. A comparison of these Proterozoic granites with Australian and Papua New Guinean granites of other time periods shows that these characteristic Sr-depleted Y-undepleted patterns are also dominant in early Palaeozoic granites. They are significantly different from those of granites in modern island arcs associated with subduction, and with most granites from Archaean terranes, where the multi-element diagrams are dominated by Sr-undepleted, Y-depleted patterns.The Sr-depleted, Y-undepleted patterns are thought to indicate source regions that contained plagioclase but not garnet, whilst the Sr-undepleted, Y-depleted patterns are taken to correspond with the presence of garnet, but not plagioclase, in the source rocks. The Sr-depleted, Y-undepleted patterns also only occur in regions where the lower crustal structure is dominated by an underplated mafic layer with a P-wave velocity of 7·2-7·-4 km/s. In contrast, in regions where the granites are dominated by Sr-undepleted, Y-depleted patterns, such as in the Archaean and in Cainozoic island arcs, this intermediate velocity layer is not present, and the crust-mantle boundary is very sharp.Two other distinctive compositional changes have been noted among the I-type granites of different age. Firstly, Na is highest in Archaean and Cainozoic granites, and lowest in early Proterozoic granites; Palaeozoic and Mesozoic granites have intermediate values. Secondly, late Archaean and Proterozoic granites are the most enriched in K, Th and U, while the Cainozoic and early Archaean tonalites are the most depleted; Palaeozoic and Mesozoic granites again contain intermediate amounts of those elements.
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Ashley, Paul M., Bernd G. Lottermoser, and Keith M. Scott. "Supergene iron phosphate minerals in Proterozoic ironstones from the Olary Block, South Australia." Neues Jahrbuch für Mineralogie - Monatshefte 1997, no. 7 (September 12, 1997): 309–27. http://dx.doi.org/10.1127/njmm/1997/1997/309.

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Дисертації з теми "Proterozoic Australia"

1

Haines, Peter W. "Carbonate shelf and basin sedimentation, late Proterozoic Wonoka Formation, South Australia /." Title page, contents and summary only, 1987. http://web4.library.adelaide.edu.au/theses/09PH/09phh152.pdf.

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Phillips, Johnnie O. "Petrology of the Late Proterozoic(?) - Early Cambrian Arumbera Sandstone and the Late Proterozoic Quandong Conglomerate, East-central Amadeus Basin, Central Australia." DigitalCommons@USU, 1986. https://digitalcommons.usu.edu/etd/6684.

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Throughout the James Ranges and Gardiner Range the Arumbera Sandstone forms prominent strike ridges with distinctive dark reddish slopes and pale red to orange-white cliffs. Because of their lithologic and stratigraphic similarities, the names Eninta and ''Quandong" for these units should be suppressed in favor of the name of Arumbera Sandstone, which has precedence. The stratigraphic and lithologic differences observed between the Quandong Conglomerate in the type locality and the Arumbera Sandstone in the study area suggest that these units are not equivalent. Similarites with the Areyonga Formation suggest the Quandong Conglomerate could be part of the Areyonga Formation. Lithofacies la, ld, and 2b, and Unit 3 of the Arumbera and its equivalents are typically recessive arkoses, subarkose, and mudrocks. They are interpreted as nearshore-marine to coastal deltaic deposits which include intertonguing tidal-flat, tidal-channel, and beach sediments. Lithofacies 1b and 2a consist of cliff-forming arkoses, subarkoses, and lithic arkoses. Lithofacies 2c is also resistant, and consists of orthoconglomerates and conglomeratic sandstones. Lithofacies 1e is moderately resistant, and consists of paraconglomerates, conglomeratic sandstones, and mudrocks. It and lithofacies 2c contain pebbles and small cobbles of chert, quartzite, vein quartz, silicified ooids, and limestone, dolostone, shale, and sandstone. These four lithofacies are interpreted as braidplain and fluvial sheet sands. In the east-central part of the Amadeus Basin the Arumbera Sandstone probably was deposited in a coastal environment as a sequence of deltaic sediments that was dominated by fluvial processes. The Arumbera Sandstone appears to be the molasse derived from the Late Proterozoic and Early Cambrian Petermann Ranges orogeny. Source rocks include sedimentary, low- to middle-rank metamorphic, and plutonic granites. Grain mineralogy and weathering characteristics suggest a hot, semiarid climate during deposition of the Arumbera. The Arumbera Sandstone and Quandong Conglomerate contain fair to good porosity and permeability, and petrographic evidence shows mesogenetic generation of secondary porosity. Previous and present burial depths are adequate for the generation of petroleum. The presence of suitable underlying .source rocks, overlying salt of the Chandler for a seal, and stratigraphic and structural traps suggest a good potential for petroleum. Production of dry gas from the lower part of the Arumbera at Dingo field, north of Deep Well Homestead, confirms the petroleum potential of this formation.
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Ogasawara, Masatsugu. "Petrology of early Proterozoic granitoids in the Halls Creek mobile zone, northern Australia /." Title page, contents and summary only, 1996. http://web4.library.adelaide.edu.au/theses/09PH/09pho34.pdf.

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Thesis (Ph. D.)--University of Adelaide, Dept. of Geology & Geophysics, 1997.
Errata pasted onto front end paper. Two folded maps in pocket on back cover. Four microfiches in pocket on back cover. Includes bibliographical references (leaves 251-289).
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Piechocka, Agnieszka Marta. "The Tectonothermal Evolution of the Gascoyne Province and its Role in Proterozoic Australia." Thesis, Curtin University, 2019. http://hdl.handle.net/20.500.11937/77388.

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SHRIMP U-Pb phosphate geochronology was used to date low- to high-grade metamorphism and leucocratic magmatism associated with Proterozoic intraplate reworking in the Gascoyne Province of Western Australia. The results show that regional metamorphism is probably related to emplacement of magmas rather than to the presence of a thermal lid as widely proposed. Late reactivation of the province, which established the present crustal architecture, was successfully dated using 40Ar/39Ar mica geochronology.
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Hapugoda, Hapugoda Udage Sarath. "Late Archaean and Early Proterozoic crustal evolution of the Georgetown Block, Northeast Queensland, Australia /." St. Lucia, Qld, 2002. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe16503.pdf.

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Hancock, S. L. "Tectonic development of the lower proterozoic basement in the Kimberley district of Northwestern Western Australia." Adelaide, 1991. http://hdl.handle.net/2440/21653.

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Baghiyan-Yazd, Mohammad Hassan. "Palaeoichnology of the terminal Proterozoic-Early Cambrian transition in central Australia : interregional correlation and palaeoecology." Title page, table of contents and abstract only, 1998. http://web4.library.adelaide.edu.au/theses/09PH/09phb1445.pdf.

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Hancock, S. L. "Tectonic development of the lower proterozoic basement in the Kimberley district of Northwestern Western Australia." Thesis, Adelaide, 1991. http://hdl.handle.net/2440/21653.

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Crowhurst, Peter V. "The geology, petrology and geochemistry of the Proterozoic Inlier, south of Myponga, Fleurieu Peninsula, South Australia /." Title page, contents and abstract only, 1988. http://web4.library.adelaide.edu.au/theses/09SB/09sbc953.pdf.

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Stewart, Kathryn. "High temperature felsic volcanism and the role of mantle magmas in proterozoic crustal growth : the Gawler Range volcanic province /." Title page, contents and abstract only, 1992. http://web4.library.adelaide.edu.au/theses/09PH/09phs8488.pdf.

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Книги з теми "Proterozoic Australia"

1

Blake, D. H., fl. 1967-, ed. Geology of the Proterozoic Davenport province, central Australia. Canberra: Australian Government Publishing Service, 1987.

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2

Zang, Wen Long. Late Proterozoic and Cambrian microfossils and biostratigraphy, Amadeus Basin, central Australia. Brisbane: Association of the Australasian Palaeontologists, 1992.

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3

Jerusalem), International Sedimentological Congress (10th 1978. Sedimentology of the Middle Proterozoic McArthur Basin, Northern Australia: 12th International Sedimentological Congress, Field Excursion 13A. Canberra, A.C.T: Bureau of Mineral Resources, Geology asnd Geophysics, 1986.

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4

Blake, D. H., fl. 1967- and Australia. Bureau of Mineral Resources, Geology and Geophysics., eds. Geology of the Proterozoic Davenport province, central Australia. Canberra: Australian Govt. Pub. Service, 1987.

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5

V, Preiss W., ed. The Adelaide geosyncline: Late Proterozoic stratigraphy, sedimentation, palaeontology and tectonics. SouthAustralia: D.J. Woolman, 1987.

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6

J, Parker A., and Geological Society of Australia. Specialist Group in Tectonics and Structural Geology., eds. Archaean - early proterozoic granitoids, metasediments and mylonites of Southern Eyre Peninsula, South Australia. Sydney, Australia: Geological Society of Australia, 1988.

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Частини книг з теми "Proterozoic Australia"

1

Finlayson, D. M. "Seismic features of Proterozoic crust in northern Australia and their evolution." In Proterozic Lithospheric Evolution, 99–113. Washington, D. C.: American Geophysical Union, 1987. http://dx.doi.org/10.1029/gd017p0099.

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2

Etheridge, M. A., R. W. R. Rutland, and L. A. I. Wyborn. "Orogenesis and tectonic process in the early to middle Proterozoic of northern Australia." In Proterozic Lithospheric Evolution, 131–47. Washington, D. C.: American Geophysical Union, 1987. http://dx.doi.org/10.1029/gd017p0131.

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3

Lindsay, John F., and 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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4

Myers, John S. "Tectonic evolution of deep crustal structures in the mid-Proterozoic Albany-Fraser Orogen, Western Australia." In Evolution of Geological Structures in Micro- to Macro-scales, 473–85. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5870-1_26.

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Glikson, A. Y., C. G. Ballhaus, B. R. Goleby, and R. D. Shaw. "Major Thrust Faults and the Vertical Zonation of the Middle to Upper Proterozoic Crust in Central Australia." In Exposed Cross-Sections of the Continental Crust, 285–304. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-0675-4_11.

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Eriksson, K. A., E. L. Simpson, and M. J. Jackson. "Stratigraphical Evolution of a Proterozoic Syn-Rift to Post-Rift Basin: Constraints on the Nature of Lithospheric Extension in the Mount Isa Inlier, Australia." In Tectonic Controls and Signatures in Sedimentary Successions, 203–21. Oxford, UK: Blackwell Publishing Ltd., 2009. http://dx.doi.org/10.1002/9781444304053.ch12.

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McCulloch, M. T. "Sm-Nd isotopic constraints on the evolution of Precambrian crust in the Australian continent." In Proterozic Lithospheric Evolution, 115–30. Washington, D. C.: American Geophysical Union, 1987. http://dx.doi.org/10.1029/gd017p0115.

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Plimer, I. R. "Tourmalinites Associated with Australian Proterozoic Submarine Exhalative Ores." In Base Metal Sulfide Deposits in Sedimentary and Volcanic Environments, 255–83. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-662-02538-3_16.

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Donnelly, T. H., and I. H. Crick. "Biological and Abiological Sulfate Reduction in Two Northern Australian Proterozoic Basins." In Early Organic Evolution, 398–407. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-76884-2_30.

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Johnson, Simon P. "Australia: Proterozoic." In Encyclopedia of Geology, 603–16. Elsevier, 2021. http://dx.doi.org/10.1016/b978-0-12-409548-9.12103-7.

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Тези доповідей конференцій з теми "Proterozoic Australia"

1

Astafieva, Marina, Richard B. Hoover, Alexei Y. Rozanov, P. Vickers-Rich, and A. Wilde. "Microbial remains in Middle Proterozoic rocks of Northern Australia." In Optical Science and Technology, the SPIE 49th Annual Meeting, edited by Richard B. Hoover, Gilbert V. Levin, and Alexei Y. Rozanov. SPIE, 2004. http://dx.doi.org/10.1117/12.558919.

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2

Thorkelson, Derek, Jacob Verbaas, Kirsti P. R. Medig, and Francesca Furlanetto. "PROTEROZOIC WILSON CYCLICITY AND ITS APPLICATION TO LAURENTIA-AUSTRALIA INTERACTIONS." In Rocky Mountain Section - 69th Annual Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017rm-293108.

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Subarkah, Darwinaji, Alan Collins, Juraj Farkas, Morgan Blades, Georgina Virgo, and Yuexiao Shao. "Reconstructing ancient palaeoenvironments from the Mid-Proterozoic packages of the greater McArthur Basin, Northern Australia." In Goldschmidt2022. France: European Association of Geochemistry, 2022. http://dx.doi.org/10.46427/gold2022.10706.

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McConachie*, Bruce A., Peter Stanmore, Lucas McLean-Hodgson, Anargul Kushkarina, and Edward Lewis. "Unconventional Gas Reservoir Productivity in Australian Proterozoic Rocks — Studies From the McArthur, Beetaloo, Mount Isa and Amadeus." 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/ice2015-2159072.

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Yoshiya, Kazumi, Yusuke Sawaki, Manabu Nishizawa, Yohei Matsui, Tsuyoshi Komiya, and Shigenori Maruyama. "NITROGEN/CARBON ISOTOPE RATIOS FROM THE EARLY TO MIDDLE PROTEROZOIC SEDIMENTARY ROCKS, MCARTHUR BASIN, NORTHERN AUSTRALIA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-281347.

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Crombez, Vincent, Marcus Kunzmann, Claudio Delle Piane, Mohinudeen Faiz, Stuart Munday, and Anne Forbes. "STRATIGRAPHIC ARCHITECTURE OF A PROTEROZOIC SHALE PLAY: INSIGHTS FROM WELL CORRELATION IN THE VELKERRI FORMATION (BEETALOO SUB-BASIN, NORTHERN TERRITORY, AUSTRALIA)." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-357071.

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Fanning, C. Mark, John W. Goodge, Christopher M. Fisher, and Jeff D. Vervoort. "AGE AND ISOTOPIC CONSTRAINTS FOR THE PROTEROZOIC EVOLUTION OF CENTRAL EAST ANTARCTICA AND RELATIONSHIP TO AUSTRALIA AND LAURENTIA IN THE COLUMBIA AND RODINIA SUPERCONTINENTS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-299618.

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Popov, Daniil, Richard Spikings, Maria Ovtcharova, Alexey Ulianov, Gary O'Sullivan, Massimo Chiaradia, David Chew, Eszter Badenszki, Stephen Daly, and Joshua Davies. "Multi-method approach to understanding the migration mechanisms of Pb in apatite and Ar in alkali feldspar from Proterozoic granitic batholiths from the Mt. Isa Inlier (Australia)." In Goldschmidt2021. France: European Association of Geochemistry, 2021. http://dx.doi.org/10.7185/gold2021.6981.

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Звіти організацій з теми "Proterozoic Australia"

1

Jarrett, A. J. M., D. Gross, B. Horsfield, and C. J. Boreham. Organic petrography of Proterozoic shales from northern Australia. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.035.

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2

Jarrett, A. J. M., D. Misch, A. H. E. Bailey, C. J. Boreham, and B. Horsfield. Qualitative BIB-SEM imaging of Proterozoic shales in northern Australia. Geoscience Australia, 2021. http://dx.doi.org/10.11636/record.2021.017.

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3

Jarrett, A. J. M., C. J. Boreham, T. J. Palu, I. Long, Z. Hong, and J. Chen. Bulk kinetics of Proterozoic kerogens from the McArthur Basin and Lawn Hill Platform, northern Australia. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.037.

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4

Thorne, Jane, Michelle Cooper, and Jonathan Claoué-Long. Guide to using the Australian mafic-ultramafic magmatic events GIS dataset: Archean, Proterozoic and Phanerozoic magmatic events. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.039.

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