Academic literature on the topic 'Musgrave Province'
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Journal articles on the topic "Musgrave Province"
Gum, J. C., and E. A. Belousova. "Musgrave Province Reconnaissance Using TerraneChrony™." ASEG Extended Abstracts 2006, no. 1 (December 2006): 1–7. http://dx.doi.org/10.1071/aseg2006ab061.
Full textWade, 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.
Full textSoerensen, Camilla, Andy Love, Tim Munday, Carmen Krapf, Adrian Costar, Kent Inverarity, Michael Gogoll, and Mat Gilfedder. "Uncovering the Musgrave Province in South Australia using airborne EM." ASEG Extended Abstracts 2018, no. 1 (December 2018): 1–5. http://dx.doi.org/10.1071/aseg2018abt5_3h.
Full textCarr, 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.
Full textJoly, 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.
Full textPollett, Alicia, Stephan Thiel, Betina Bendall, Tom Raimondo, and Martin Hand. "Mapping the Gawler Craton–Musgrave Province interface using integrated heat flow and magnetotellurics." Tectonophysics 756 (April 2019): 43–56. http://dx.doi.org/10.1016/j.tecto.2019.02.017.
Full textKarykowski, 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.
Full textPERKINS, PHILIP D. "New species (130) of the hyperdiverse aquatic beetle genus Hydraena Kugelann from Papua New Guinea, and a preliminary analysis of areas of endemism (Coleoptera: Hydraenidae)." Zootaxa 2944, no. 1 (June 8, 2011): 1. http://dx.doi.org/10.11646/zootaxa.2944.1.1.
Full textSchwarz, A., and S. Constable. "Structural and geochemical characteristics of the Ngunala Intrusion of the Giles Complex, Musgrave Province, South Australia." Applied Earth Science 116, no. 4 (December 2007): 201–14. http://dx.doi.org/10.1179/174327507x272003.
Full textSmithies, R. H., C. L. Kirkland, F. J. Korhonen, A. R. A. Aitken, H. M. Howard, W. D. Maier, M. T. D. Wingate, R. Quentin de Gromard, and K. Gessner. "The Mesoproterozoic thermal evolution of the Musgrave Province in central Australia — Plume vs. the geological record." Gondwana Research 27, no. 4 (June 2015): 1419–29. http://dx.doi.org/10.1016/j.gr.2013.12.014.
Full textDissertations / Theses on the topic "Musgrave Province"
Wade, Benjamin P. "Unravelling the tectonic framework of the Musgrave Province, Central Australia." 2006. http://hdl.handle.net/2440/57768.
Full texthttp://proxy.library.adelaide.edu.au/login?url= http://library.adelaide.edu.au/cgi-bin/Pwebrecon.cgi?BBID=1261003
Thesis(PhD)-- University of Adelaide, School of Earth and Environmental Sciences, 2006
Wade, Benjamin P. "Unravelling the tectonic framework of the Musgrave Province, Central Australia." Thesis, 2006. http://hdl.handle.net/2440/57768.
Full textThesis (Ph.D.) -- University of Adelaide, School of Earth and Environmental Sciences, 2006
Telenko, B. "High pressure metamorphism during intracratonic orogenesis: physical conditions and rates from the Amata region, Musgrave Province." Thesis, 2010. http://hdl.handle.net/2440/106276.
Full textThe intracratonic orogenesis of the Petermann Orogeny caused the formation of high-pressure, low-geothermal gradient, eclogite facies rocks. These geologically rare rocks are found in the exposed orogenic core, observable near the Traditional community of Amata, in the Musgrave Province. Their formation remains a mystery and as a result two contrasting models have been proposed to explain their formation; namely whether orogenesis occurred in “hot” crust and was long lived, or occurred in “cold” crust and was short-lived. In situ LA-ICP-MS analysis of monazite show that metamorphism occurred at c. 598 Ma. Using conventional thermobarometric techniques, peak conditions are estimated to have reached ~640 °C and ~11.5 kbar. Integrating this data with petrological observations and calculated P-T pseudosections, a clock-wise P-T path was defined, which is typical of an orogenic setting. Diffusion modelling using garnet compositional profiles from grains of both relict composition and those interpreted to be reset, estimated the minimum duration for prograde metamorphism to be ~27 Myr. The same garnet grains show little to no evidence of cooling/exhumation, which has been attributed to the low metamorphic peak temperature. Results of this study make a direct contribution to two contrasting models for orogenesis. Combining new evidence from this study with tectonothermal evidence from the western Musgrave Province and sedimentological data from the Officer Basin to the south, it is concluded that shear heating (or short-lived deformation) is not a plausible model for Petermann-aged deformation. Despite the lack of spatially continuous data across the Musgrave Province, long-lived orogenesis is the more supported model in light of new evidence emerging from this study.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2010
Wong, Y. H. "Detrital constraints on the southern Amadeus Basin –new analysis of zircon and apatite samples for detrital provenance and thermal evolution." Thesis, 2018. https://hdl.handle.net/2440/133693.
Full textThe Amadeus Basin is a Late Proterozoic to early Phanerozoic basin in central Australia, which records a complex sedimentation and thermal history throughout the basin. This study presents new analysis of zircon and apatite samples for detrital provenance and thermal evolution, focused in the southern Amadeus Basin (KULGERA). While the thermal history and provenance are well constrained for the north, such data for the southern region of the basin are lacking. Nineteen outcrop samples are analysed for detrital zircon U-Pb and provenance and one BR05DD01 drill-core sample is analysed for the AUPb and AFT ages. All sampled zircons share a similar prominent peak at ca. 1086 – 1163 Ma and a second prominent peak at ca. 1554 – 1791 Ma. However, all formations do not share a similar provenance due to the major tectonic events from the Musgrave Province and Arunta Region influencing sedimentation and architecture in the Amadeus Basin. Two age peaks derived in the AFT plot at114 +/- 11 Ma and 223 +/- 13 Ma suggest an extensive thermal history in the apatite partial annealing zone. Due to the insufficient number of analysed apatite grains, this hinders the identification of age populations and more detailed age calculations. More data would be required for the apatite analysis in order to conclude a specified age population and age calculation.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, YEAR
Walsh, A. K. "Duration of the Petermann Orogeny from coupled diffusion and phase equilibria modelling." Thesis, 2010. http://hdl.handle.net/2440/106280.
Full textThe Ediacaran to Cambrian (600-500 Ma) intraplate Petermann Orogeny significantly affected the crustal architecture of Central Australia, resulting in the exhumation of the Musgrave Province from beneath the Centralian Superbasin. In the western Musgrave Province response to intensive deformation is variable, with pervasive mylonitic reworking and localised migmitisation in the western Mann Ranges, and discrete mylonitisation in the eastern Mann Ranges. The duration of this period of intraplate orogenesis is a currently debated topic. Ti-in-zircon thermometry coupled with SHRIMP U-Pb zircon geochronology indicate that peak temperatures of 733±23°C in the western Mann Ranges occurred at circa 540 Ma. Combined diffusion-cooling modelling, U-Pb rutile and titanite isotopic data and calculated phase equilibria of recrystallised metagranites from the Cockburn Shear Zone and kyanite-bearing mylonites from the Mt. Charles Thrust indicate exhumation driven cooling from peak P-T conditions of 12-14 kbars and 700-750°C to 6-7 kbars and 550-600°C at c. 500 Ma occurred at a rate of 3.75-5.6°C/ My. These results indicate a slow-cooling and long-lived thermal regime and additionally suggests that final exhumation of the Musgrave Province had not occurred by c. 500 Ma, much younger than previously estimated. These findings suggest that granulite-facies metamorphism in the Musgrave Province was regional and that other factors such as fluid, control the variations in style of structural reworking. This study lends support to the notion that the intraplate Petermann Orogeny was long-lived and does not advocate short-lived orogenesis or the theory that shear heating is the driving force for metamorphism.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2010
Oertel, A. G. "Magnetotelluric survey of the Central Australian Craton, with a focus on the structural history of the Warumpi and Musgrave Provinces and the Arunta Complex." Thesis, 2013. http://hdl.handle.net/2440/106295.
Full textIn spite of the continent of Australia being the oldest and most tectonically stable on Earth, its structural history is still the subject of much conjecture. The final closure of the South Australian Craton with the North Australian Craton at roughly 1080 million years ago deformed much of Central Australia into the lithospheric arrangement observed today. Structural constraints have been developed in the last 30 years on the history of the Musgrave Province, Amadeus Basin, Warumpi Province and Arunta Complex in the southern part of the Northern Territory. In this study the resistivity structure of these four provinces was assessed through the use of a long-period magnetotelluric survey along the Stuart Highway from the South Australia-Northern Territory border to 90 kilometres north of Alice Springs. A key focus was to determine whether the structural arrangement, identified in a magnetotelluric survey conducted 100 kilometres to the east of this profile in 2006, is laterally consistent between the four provinces. In the Stuart Highway profile model the major structures present exhibit a different arrangement, particularly in the northern part of the profile, resulting in the conclusion that the mechanism for the lithospheric closure of the region was a more complex nature than was previously thought.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2013
Books on the topic "Musgrave Province"
Pugh, Brian A., and Ronny Frith. Chaos and Compromise. University Press of Mississippi, 2020. http://dx.doi.org/10.14325/mississippi/9781496830197.001.0001.
Full textConference papers on the topic "Musgrave Province"
Connelly, Daniel P., Arif M. Sikder, Joseph B. McGee Turner, Tina R. Hill, and Jose Brum. "GEOCHEMICAL CHARACTERISTICS OF THE PSEUDOTACHYLITES OF MUSGRAVE PROVINCE." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-339152.
Full textConnelly, Daniel P., and Arif M. Sikder. "SHOCK FEATURES IN MINERAL GRAINS FROM PSEUDOTACHYLITE BRECCIA OF THE MUSGRAVE PROVINCE AUSTRALIA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-323970.
Full textAlexander, Elinor. "Natural hydrogen exploration in South Australia." In PESA Symposium Qld 2022. PESA, 2022. http://dx.doi.org/10.36404/putz2691.
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