Готові списки джерел за темами / Unconformities (Geology) South Australia Tirrawarra Field

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Добірка наукової літератури з теми "Unconformities (Geology) South Australia Tirrawarra Field"

Автор: Grafiati
Опубліковано: 4 червня 2021
Оновлено: 31 січня 2023

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Статті в журналах з теми "Unconformities (Geology) South Australia Tirrawarra Field"

1

Xue, Er-Kun, Wei Wang, Mei-Fu Zhou, Manoj K. Pandit, Si-Fang Huang, and Gui-Mei Lu. "Late Neoproterozoic–early Paleozoic basin evolution in the Cathaysia Block, South China: Implications of spatio-temporal provenance changes on the paleogeographic reconstructions in supercontinent cycles." GSA Bulletin 133, no. 3-4 (August 4, 2020): 717–39. http://dx.doi.org/10.1130/b35588.1.

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Abstract The role of the Cathaysia Block, South China, and its linkage with orogenesis in the Rodinia and Gondwana supercontinents remain unresolved because of uncertainties in its paleoposition in supercontinental reconstructions. The lithostratigraphic, geochronologic, geochemical (including isotopic), and paleocurrent data on late Neoproterozoic to early Paleozoic sub-basins in the Cathaysia Block reveal spatio-temporal, tectono-sedimentary, and provenance diversity that show linkages with previously adjacent terranes and orogens in East Gondwana. An abundance of siliceous and conglomeratic rocks, local unconformities, and pinch-out in certain layers indicate a late Cryogenian proximal deposition, late Ediacaran transgression, and Middle Cambrian uplift. Cryogenian to early Ordovician strata contain predominantly 1000–900 Ma (late Grenvillian age) detrital zircon population, whereas 1300–1050 Ma (early Grenvillian age) zircons are only dominant in strata earlier than late Ediacaran. Besides, 850–700 Ma zircons are the most prominent group in the Middle Cambrian strata along with an occasional increase in the 650–500 Ma (Pan-African age) zircons. The Grenvillian age zircon groups exhibit significant sediment input from the eastern Indian terrane (990–950 Ma) and western Australia (1300–1050 Ma), underlining the fact that the Cathaysia Block was located between these two terranes in the northern part of East Gondwana. The diminishing contribution of early Grenvillian components in the late Ediacaran strata can be linked to the Pinjarra Orogeny (550–520 Ma), which led to uplift that blocked the transport of detritus from Australia. Middle Cambrian provenance variation with high abundance of 850–700 Ma components indicates the presence of intrinsic sediment from the Wuyishan terrane of South China. Given that the Cathaysia Block was a passive continental margin, this change was caused by the uplift of the southeastern Cathaysia Block, which was related to the far-field stress effects of the late phase of the Kuunga Orogeny (530–480 Ma). The decrease in abundance of early Grenvillian and Pan-African zircons in space implies that they were transported into the basins through independent drainage systems. This is consistent with the local and temporal variations in paleocurrent orientations during the Cambrian, further implying diverse and complex drainage systems in the southwestern Cathaysia Block during this period.
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H. Scott Hamlin (2), Shirley P. Dut. "Depositional Controls on Reservoir Properties in a Braid-Delta Sandstone, Tirrawarra Oil Field, South Australia." AAPG Bulletin 80 (1996). http://dx.doi.org/10.1306/64ed876e-1724-11d7-8645000102c1865d.

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J. M. Bever, P. G. Carroll, E. W. W. "Core Facies, Petrology, and Permeability of Tirrawarra Sandstone, Moorari Field, Cooper Basin, South Australia: ABSTRACT." AAPG Bulletin 72 (1988). http://dx.doi.org/10.1306/703c8335-1707-11d7-8645000102c1865d.

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Scott H. Hamlin, Shirley P. Dutton,. "Resource Optimization through Facies-Based Characterization of a Braid-Delta Sandstone Reservoir, Tirrawarra Oil Field, Cooper Basin, South Australia: ABSTRACT." AAPG Bulletin 78 (1994). http://dx.doi.org/10.1306/a260004d-171b-11d7-8645000102c1865d.

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Дисертації з теми "Unconformities (Geology) South Australia Tirrawarra Field"

1

Kennedy, Sean. "A study of the Patchawarra Formation, Tirrawarra Field, Southern Cooper Basin, South Australia." Title page, contents and abstract only, 1988. http://web4.library.adelaide.edu.au/theses/09SM/09smk36.pdf.

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Cubitt, Chris. "Controls on reservoir development and quality in a glacial sequence; a study of the late palaeozoic, Cooper Basin South Australia and Queensland, Australia : thesis submitted to the University of Adelaide in fullfillment [sic] of the requirement for the Degree of Doctor of Philosophy, July 2000." Title page, contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09PH/09phc962.pdf.

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At head of title: National Centre for Petroleum Geology and Geophysics. CD-ROM contains Appendices (1-10) in PDF. Includes copies of papers co-authored by the author. Includes bibliographical references (leaves [471]-499 in vol. 2) Studies the provenance and diagenesis of the Merrimelia Formation in South Australia and Queensland; a complex mosaic of glacial facies in which the Tirrawarra Sandstone and Merrimelia Formation exhibit an interfingering relationship, and defines the relationship further. Indicates that the Tirrawarra Sandstone should be included in the Merrimelia Formation as a "facies type" as both the Merrimelia and Tirrawarra sediments form an integrated suite of sediments. System requirements for accompanying CD-ROM: Macintosh or IBM compatible computer with Windows NT. Other requirements: Adobe Acrobat Reader.
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Cubitt, Chris, and National Centre for Petroleum Geology &amp Geophysics (Australia). "Controls on reservoir development and quality in a glacial sequence; a study of the late palaeozoic, Cooper Basin South Australia and Queensland, Australia : thesis submitted to the University of Adelaide in fullfillment [sic] of the requirement for the Degree of Doctor of Philosophy, July 2000 / Chris Cubitt." 2000. http://hdl.handle.net/2440/21707.

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Анотація:
At head of title: National Centre for Petroleum Geology and Geophysics.
CD-ROM contains Appendices (1-10) in PDF.
Includes copies of papers co-authored by the author.
Includes bibliographical references (leaves [471]-499 in vol. 2)
System requirements for accompanying CD-ROM: Macintosh or IBM compatible computer with Windows NT. Other requirements: Adobe Acrobat Reader.
2 v. (various pagings) : ill. (some col.), maps, ports. ; 30 cm. + 1 CD-ROM (4 3/4 in.)
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
Studies the provenance and diagenesis of the Merrimelia Formation in South Australia and Queensland; a complex mosaic of glacial facies in which the Tirrawarra Sandstone and Merrimelia Formation exhibit an interfingering relationship, and defines the relationship further. Indicates that the Tirrawarra Sandstone should be included in the Merrimelia Formation as a "facies type" as both the Merrimelia and Tirrawarra sediments form an integrated suite of sediments.
Thesis (Ph.D.)--University of Adelaide, Dept. of Geology, 2000?
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Cubitt, Chris, and National Centre for Petroleum Geology &amp Geophysics (Australia). "Controls on reservoir development and quality in a glacial sequence; a study of the late palaeozoic, Cooper Basin South Australia and Queensland, Australia : thesis submitted to the University of Adelaide in fullfillment [sic] of the requirement for the Degree of Doctor of Philosophy, July 2000 / Chris Cubitt." Thesis, 2000. http://hdl.handle.net/2440/21707.

Повний текст джерела
Анотація:
At head of title: National Centre for Petroleum Geology and Geophysics.
CD-ROM contains Appendices (1-10) in PDF.
Includes copies of papers co-authored by the author.
Includes bibliographical references (leaves [471]-499 in vol. 2)
System requirements for accompanying CD-ROM: Macintosh or IBM compatible computer with Windows NT. Other requirements: Adobe Acrobat Reader.
2 v. (various pagings) : ill. (some col.), maps, ports. ; 30 cm. + 1 CD-ROM (4 3/4 in.)
Studies the provenance and diagenesis of the Merrimelia Formation in South Australia and Queensland; a complex mosaic of glacial facies in which the Tirrawarra Sandstone and Merrimelia Formation exhibit an interfingering relationship, and defines the relationship further. Indicates that the Tirrawarra Sandstone should be included in the Merrimelia Formation as a "facies type" as both the Merrimelia and Tirrawarra sediments form an integrated suite of sediments.
Thesis (Ph.D.)--University of Adelaide, Dept. of Geology, 2000?
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