Relevant bibliographies by topics / West Musgrave

Academic literature on the topic 'West Musgrave'

Author: Grafiati
Published: 4 June 2021
Last updated: 19 February 2022

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Journal articles on the topic "West Musgrave"

1

Wade, B. P., D. E. Kelsey, M. Hand, and K. M. Barovich. "The Musgrave Province: Stitching north, west and south Australia." Precambrian Research 166, no. 1-4 (October 2008): 370–86. http://dx.doi.org/10.1016/j.precamres.2007.05.007.

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Hatley, Allen G., Karen Holliday Tanner, and John D. Tanner,. "Last of the Old-Time Outlaws: The George West Musgrave Story." Western Historical Quarterly 34, no. 3 (October 1, 2003): 399. http://dx.doi.org/10.2307/25047337.

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3

Cameron, Alick. "A West Country polymath: William Musgrave MD FRS FRCP, of Exeter (1655–1721)." Journal of Medical Biography 6, no. 3 (August 1998): 166–70. http://dx.doi.org/10.1177/096777209800600310.

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4

Joly, Aurore, Alan Aitken, Mike Dentith, TC McCuaig, Alok Porwal, Hugh Smithies, Ian Tyler, and Shane Evans. "Architecture and evolution of the West Musgrave Province, and implications for mineral prospectivity." ASEG Extended Abstracts 2012, no. 1 (December 2012): 1–4. http://dx.doi.org/10.1071/aseg2012ab204.

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5

Karykowski, Bartosz T., Paul A. Polito, Wolfgang D. Maier, and Jens Gutzmer. "Origin of Cu-Ni-PGE Mineralization at the Manchego Prospect, West Musgrave Province, Western Australia." Economic Geology 110, no. 8 (November 9, 2015): 2063–85. http://dx.doi.org/10.2113/econgeo.110.8.2063.

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6

Carr, Lidena, Russell Korsch, Arthur Mory, Roger Hocking, Sarah Marshall, Ross Costelloe, Josef Holzschuh, and Jenny Maher. "Structural and stratigraphic architecture of Australia's frontier onshore sedimentary basins: the Western Officer and Southern Carnarvon basins, Western Australia." APPEA Journal 52, no. 2 (2012): 670. http://dx.doi.org/10.1071/aj11084.

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During the past five years, the Onshore Energy Security Program, funded by the Australian Government and conducted by Geoscience Australia, in conjunction with state and territory geological surveys, has acquired deep seismic reflection data across several frontier sedimentary basins to stimulate petroleum exploration in onshore Australia. This extended abstract presents data from two seismic lines collected in Western Australia in 2011. The 487 km long Yilgarn-Officer-Musgrave (YOM) seismic line crossed the western Officer Basin in Western Australia, and the 259 km long, Southern Carnarvon Seismic line crossed the Byro Sub-basin of the Southern Carnarvon Basin. The YOM survey imaged the Neoproterozoic to Devonian western Officer Basin, one of Australia's underexplored sedimentary basins with hydrocarbon potential. The survey data will also provide geoscientific knowledge on the architecture of Australia's crust and the relationship between the eastern Yilgarn Craton and the Musgrave Province. The Southern Carnarvon survey imaged the onshore section of the Ordovician to Permian Carnarvon Basin, which offshore is one of Australia's premier petroleum-producing provinces. The Byro Sub-basin is an underexplored depocentre with the potential for both hydrocarbon and geothermal energy. Where the seismic traverse crossed the Byro Sub-basin it imaged two relatively thick half graben, on west dipping bounding faults. Structural and sequence stratigraphic interpretations of the two seismic lines are presented in this extended abstract.
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Howard, H. M., R. H. Smithies, C. L. Kirkland, D. E. Kelsey, A. Aitken, M. T. D. Wingate, R. Quentin de Gromard, C. V. Spaggiari, and W. D. Maier. "The burning heart — The Proterozoic geology and geological evolution of the west Musgrave Region, central Australia." Gondwana Research 27, no. 1 (January 2015): 64–94. http://dx.doi.org/10.1016/j.gr.2014.09.001.

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8

Kirkland, Christopher L., R. Hugh Smithies, Ailsa J. Woodhouse, Heather M. Howard, Michael T. D. Wingate, Elena A. Belousova, John B. Cliff, Rosanna C. Murphy, and Catherine V. Spaggiari. "Constraints and deception in the isotopic record; the crustal evolution of the west Musgrave Province, central Australia." Gondwana Research 23, no. 2 (March 2013): 759–81. http://dx.doi.org/10.1016/j.gr.2012.06.001.

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9

Williams, Harold, R. T. Gillespie, and Otto Van Breemen. "A late Precambrian rift-related igneous suite in western Newfoundland." Canadian Journal of Earth Sciences 22, no. 11 (November 1, 1985): 1727–35. http://dx.doi.org/10.1139/e85-181.

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A granite that yields a U–Pb zircon age of 602 ± 10 Ma is associated with mafic and silicic volcanic rocks and metamorphic equivalents near Deer Lake in western Newfoundland. The granitic rocks are named the Round Pond granite, and the combined granite–volcanic suite is assigned to the Hughes Lake complex. All of the rocks are contained in the Hughes Lake structural slice that occurs above other allochthonous rocks and the autochthonous Cambrian–Ordovician carbonate sequence of western Newfoundland.The Round Pond granite is cut by metadiabase dykes. Mafic volcanic rocks, interpreted as coeval with the dykes, occur along the southeast side of the granite. A thick sequence of arkosic metagreywackes and psammitic to pelitic schists of the Mount Musgrave Group occurs stratigraphically above the mafic volcanic rocks. Regional correlations imply that the Mount Musgrave Group is of late Precambrian – Early Cambrian age, thus setting an upper stratigraphic limit to the age of the Hughes Lake complex.Perthitic and granophyric textures and the chemistry of the Round Pond granite are typical of anorogenic high-level hypersolvus intrusions. Nearby pink silicic volcanic rocks are probably consanguineous with the granite and together with the mafic volcanics form a bimodal suite.Bimodal volcanic suites and related mafic dykes and granitic intrusions imply rift tectonic settings. Occurrences along the west flank of the Appalachian Orogen are equated with the initiation of an ancient continental margin and the opening of an Iapetus Ocean. The 602 ± 10 Ma age of the Round Pond granite dates the rifting in western Newfoundland. Older isotopic ages on similar rocks in the southern Appalachians of the United States suggest a diachronous Precambrian rifting and Iapetus opening that propagated northward, much like the Mesozoic opening of the North Atlantic Ocean.
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10

Seat, Zoran, Stephen W. Beresford, Benjamin A. Grguric, Rob S. Waugh, Jon M. A. Hronsky, M. A. Mary Gee, David I. Groves, and Charter I. Mathison. "Architecture and emplacement of the Nebo–Babel gabbronorite-hosted magmatic Ni–Cu–PGE sulphide deposit, West Musgrave, Western Australia." Mineralium Deposita 42, no. 6 (February 27, 2007): 551–81. http://dx.doi.org/10.1007/s00126-007-0123-9.

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Dissertations / Theses on the topic "West Musgrave"

1

Seat, Zoran. "Geology, petrology, mineral and whole-rock chemistry, stable and radiogenic isotope systematics and Ni-Cu-PGE mineralisation of the Nebo-Babel intrusion, West Musgrave, Western Australia." University of Western Australia. School of Earth and Geographical Sciences, 2008. http://theses.library.uwa.edu.au/adt-WU2008.0202.

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The Nebo-Babel Ni-Cu-platinum-group element (PGE) magmatic sulphide deposit, a world-class ore body, is hosted in low-MgO, tube-like (chonolithic) gabbronorite intrusion in the West Musgrave Block, Western Australia. The Nebo-Babel deposit is the first significant discovery of a nickel sulphide deposit associated with the ca. 1078 Ma Giles Complex, which is part of the Warakurna large igneous province (LIP), now making the Musgrave Block a prime target for nickel sulphide exploration. The Musgrave Block is a Mesoproterozoic, east-west trending, orogenic belt in central Australia consisting of amphibolite and granulite facies basement gneisses with predominantly igneous protoliths. The basement lithologies have been intruded by mafic-ultramafic and felsic rocks; multiply deformed and metamorphosed between 1600 Ma and 500 Ma. The Giles Complex, which is part of the Warakurna LIP, was emplaced at ca. 1078 Ma and consists of a suite of layered mafic-ultramafic intrusions, mafic and felsic dykes and temporally associated volcanic rocks and granites. The Giles Complex intrusions are interpreted to have crystallised at crustal depths between 15km and 30km and are generally undeformed and unmetamorphosed.
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Books on the topic "West Musgrave"

1

1943-, Tanner John D., ed. Last of the old-time outlaws: The George West Musgrave story. Norman: University of Oklahoma Press, 2002.

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2

Musgrave, Duane. A history of the Moses Musgrave family, Quakers, Pennsylvania, Virginia, Tennessee, Kentucky, Illinois, Kansas, and further West. Kansas City, Mo. (211 West 51st St., Kansas City 64112-2431): D. and M.W. Musgrave, 1998.

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3

Jr, Tanner John D., and Karen Holliday Tanner. Last of the Old-Time Outlaws: The George West Musgrave Story. University of Oklahoma Press, 2014.

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