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Добірка наукової літератури з теми "Metamorphism (Geology) Queensland Georgetown Inlier"

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

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Статті в журналах з теми "Metamorphism (Geology) Queensland Georgetown Inlier"

1

WITHNALL, I., J. BAIN, J. DRAPER, D. MACKENZIE, and B. OVERSBY. "Proterozoic stratigraphy and tectonic history of the Georgetown Inlier, northeastern Queensland." Precambrian Research 40-41 (October 1988): 429–46. http://dx.doi.org/10.1016/0301-9268(88)90079-4.

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2

Offler, R., G. Phillips, C. L. Fergusson, and T. J. Green. "Tectonic Implications of Early Paleozoic Metamorphism in the Anakie Inlier, Central Queensland, Australia." Journal of Geology 119, no. 5 (September 2011): 467–85. http://dx.doi.org/10.1086/661191.

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3

Murgulov, Valeria, Eloise Beyer, William L. Griffin, Suzanne Y. O’Reilly, Steven G. Walters, and Darren Stephens. "Crustal evolution in the Georgetown Inlier, North Queensland, Australia: a detrital zircon grain study." Chemical Geology 245, no. 3-4 (November 2007): 198–218. http://dx.doi.org/10.1016/j.chemgeo.2007.08.001.

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4

Baker, Michael J., Anthony J. Crawford, and Ian W. Withnall. "Geochemical, Sm–Nd isotopic characteristics and petrogenesis of Paleoproterozoic mafic rocks from the Georgetown Inlier, north Queensland: Implications for relationship with the Broken Hill and Mount Isa Eastern Succession." Precambrian Research 177, no. 1-2 (February 2010): 39–54. http://dx.doi.org/10.1016/j.precamres.2009.11.003.

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5

Cave, Bradley, Richard Lilly, Stijn Glorie, and Jack Gillespie. "Geology, Apatite Geochronology, and Geochemistry of the Ernest Henry Inter-Lens: Implications for a Re-Examined Deposit Model." Minerals 8, no. 9 (September 13, 2018): 405. http://dx.doi.org/10.3390/min8090405.

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Анотація:
The Ernest Henry Iron-Oxide-Copper-Gold deposit is the largest known Cu-Au deposit in the Eastern Succession of the Proterozoic Mount Isa Inlier, NW Queensland. Cu-Au mineralization is hosted in a K-feldspar altered breccia, bounded by two major pre-mineralization shear zones. Previous research suggests that Cu-Au mineralization and the ore-bearing breccia formed simultaneously through an eruption style explosive/implosive event, facilitated by the mixing of fluids at ~1530 Ma. However, the preservation of a highly deformed, weakly mineralized, pre-mineralization feature (termed the Inter-lens) within the orebody indicates that this model must be re-examined. The paragenesis of the Inter-lens is broadly consistent with previous studies on the deposit, and consists of albitization; an apatite-calcite-quartz-garnet assemblage; biotite-magnetite ± garnet alteration; K-feldspar ± hornblende alteration; Cu-Au mineralization and post-mineralization alteration and veining. Apatite from the paragenetically early apatite-calcite-quartz-garnet assemblage produce U–Pb ages of 1584 ± 22 Ma and 1587 ± 22 Ma, suggesting that the formation of apatite, and the maximum age of the Inter-lens is synchronous with D2 deformation of the Isan Orogeny and regional peak-metamorphic conditions. Apatite rare earth element-depletion trends display: (1) a depletion in rare earth elements evenly, corresponding with an enrichment in arsenic and (2) a selective light rare earth element depletion. Exposure to an acidic NaCl and/or CaCl2-rich sedimentary-derived fluid is responsible for the selective light rare earth element-depletion trend, while the exposure to a neutral to alkaline S, Na-, and/or Ca-rich magmatic fluid resulted in the depletion of rare earth elements in apatite evenly, while producing an enrichment in arsenic. We suggest the deposit experienced at least two hydrothermal events, with the first event related to peak-metamorphism (~1585 Ma) and a subsequent event related to the emplacement of the nearby (~1530 Ma) Williams–Naraku Batholiths. Brecciation resulted from competency contrasts between ductile metasedimentary rocks of the Inter-lens and surrounding shear zones against the brittle metavolcanic rocks that comprise the ore-bearing breccia, providing permeable pathways for the subsequent ore-bearing fluids.
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Дисертації з теми "Metamorphism (Geology) Queensland Georgetown Inlier"

1

Deegan, Blake Mathew Spurway. "The petrogenesis and geochronology of lower crustal xenoliths from the Georgetown inlier, North Queensland." Thesis, Queensland University of Technology, 2020. https://eprints.qut.edu.au/204210/2/Blake_Deegan_Thesis.pdf.

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The only method of sampling the present day lower continental crust is through volcanic eruptions that transport samples of country rock to the surface. The composition, mineralogy, and age of three lower crustal xenoliths were examined from a preserved volcanic edifice, Hill 32, which erupted in North Queensland. It was found that all three samples represented former feldspathic orthogneisses. Through zircon U-Pb geochronology, the samples were found to have been subject to intense metamorphism and anatectic melting approximately 260Ma. Through rutile U-Pb geochronology, the eruption of Hill 32 in North Queensland was quantitatively dated to have erupted 1.5Ma.
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McLaren, Sandra. "The role of internal heat production during metamorphism of the Eastern Arunta Complex, central Australia, and the Mount Isa Inlier, Queensland /." Title page, contents and abstract only, 1996. http://web4.library.adelaide.edu.au/theses/09SB/09sbm161.pdf.

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Анотація:
Thesis (B. Sc.(Hons.))--University of Adelaide, Dept. of Geology and Geophysics, 1997?
National Grid reference SF53-14 (Alice Springs), SF54-1 (Mount Isa) (1:250 000). Includes bibliographical references (leaves [32-36]).
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3

McLaren, Sandra N. (Sandra Noeline). "Long-term consequences of the redistribution of heat producing elements within the continental crust: Australian examples / Sandra N. McLaren." 2001. http://hdl.handle.net/2440/19839.

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Анотація:
Includes copies of articles co-authored by author during the preparation of this thesis in back pocket.
Includes bibliographical references (leaves 113-124).
viii, 172 leaves : ill. (some col.), maps ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
Focuses on the impact of change in the distribution of heat producing elements on lithospheric thermal regimes and on temperature dependent processes such as metamorphism, magmatism and deformation, with application to Proteozoic Australia (Mount Isa and Mount Painter inliers).
Thesis (Ph.D.)--Adelaide University, Dept. of Geology and Geophysics, 2001
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4

McLaren, Sandra N. (Sandra Noeline). "Long-term consequences of the redistribution of heat producing elements within the continental crust: Australian examples / Sandra N. McLaren." Thesis, 2001. http://hdl.handle.net/2440/19839.

Повний текст джерела
Анотація:
Includes copies of articles co-authored by author during the preparation of this thesis in back pocket.
Includes bibliographical references (leaves 113-124).
viii, 172 leaves : ill. (some col.), maps ; 30 cm.
Focuses on the impact of change in the distribution of heat producing elements on lithospheric thermal regimes and on temperature dependent processes such as metamorphism, magmatism and deformation, with application to Proteozoic Australia (Mount Isa and Mount Painter inliers).
Thesis (Ph.D.)--Adelaide University, Dept. of Geology and Geophysics, 2001
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Книги з теми "Metamorphism (Geology) Queensland Georgetown Inlier"

1

Withnall, I. W. Precambrian and Palaeozoic geology of the southeastern Georgetown InLier, North Queensland. Brisbane, Qld: Queensland Dept. of Mines, 1989.

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