Добірка наукової літератури з теми "Petermann Orogeny"
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Статті в журналах з теми "Petermann Orogeny"
Perincek, D. "THE AGE OF NEOPROTEROZOIC-PALAEOZOIC SEDIMENTS WITHIN THE OFFICER BASIN OF THE CENTRALIAN SUPER-BASIN CAN BE CONSTRAINED BY MAJOR SEQUENCE-BOUNDING UNCONFORMITIES." APPEA Journal 36, no. 1 (1996): 350. http://dx.doi.org/10.1071/aj95019.
Повний текст джерелаBache, Francois, Paul Walshe, Juergen Gusterhuber, Sandra Menpes, Mattilda Sheridan, Sergey Vlasov, and Lance Holmes. "Exploration of the south-eastern part of the Frontier Amadeus Basin, Northern Territory, Australia." APPEA Journal 58, no. 1 (2018): 190. http://dx.doi.org/10.1071/aj17221.
Повний текст джерелаHawemann, Friedrich, Neil S. Mancktelow, Sebastian Wex, Alfredo Camacho, and Giorgio Pennacchioni. "Pseudotachylyte as field evidence for lower-crustal earthquakes during the intracontinental Petermann Orogeny (Musgrave Block, Central Australia)." Solid Earth 9, no. 3 (May 9, 2018): 629–48. http://dx.doi.org/10.5194/se-9-629-2018.
Повний текст джерелаScrimgeour and Close. "Regional high-pressure metamorphism during intracratonic deformation: the Petermann Orogeny, central Australia." Journal of Metamorphic Geology 17, no. 5 (September 1999): 557–72. http://dx.doi.org/10.1046/j.1525-1314.1999.00217.x.
Повний текст джерелаWalsh, A. K., T. Raimondo, D. E. Kelsey, M. Hand, H. L. Pfitzner, and C. Clark. "Duration of high-pressure metamorphism and cooling during the intraplate Petermann Orogeny." Gondwana Research 24, no. 3-4 (November 2013): 969–83. http://dx.doi.org/10.1016/j.gr.2012.09.006.
Повний текст джерелаWex, Sebastian, Neil S. Mancktelow, Friedrich Hawemann, Alfredo Camacho, and Giorgio Pennacchioni. "Inverted distribution of ductile deformation in the relatively “dry” middle crust across the Woodroffe Thrust, central Australia." Solid Earth 9, no. 4 (July 11, 2018): 859–78. http://dx.doi.org/10.5194/se-9-859-2018.
Повний текст джерелаMoussavi-Harami, R., and D. I. Gravestock. "BURIAL HISTORY OF THE EASTERN OFFICER BASIN, SOUTH AUSTRALIA." APPEA Journal 35, no. 1 (1995): 307. http://dx.doi.org/10.1071/aj94019.
Повний текст джерелаAitken, Alan R. A., Peter G. Betts, and Laurent Ailleres. "The architecture, kinematics, and lithospheric processes of a compressional intraplate orogen occurring under Gondwana assembly: The Petermann orogeny, central Australia." Lithosphere 1, no. 6 (December 2009): 343–57. http://dx.doi.org/10.1130/l39.1.
Повний текст джерелаAitken, Alan. "The architecture, kinematics, and lithospheric processes of a compressional intraplate orogen occurring under Gondwana assembly: The Petermann orogeny, central Australia." Lithosphere 1, no. 6 (December 1, 2009): 343–57. http://dx.doi.org/10.1130/l39.s1.
Повний текст джерелаAitken, Alan. "The architecture, kinematics, and lithospheric processes of a compressional intraplate orogen occurring under Gondwana assembly: The Petermann orogeny, central Australia." Lithosphere 1, no. 6 (December 1, 2009): 343–57. http://dx.doi.org/10.1130/l39.s2.
Повний текст джерелаДисертації з теми "Petermann Orogeny"
Wade, Benjamin Paul. "Nd isotopic and geochemical constraints on provenance of sedimentary rocks in the Officer Basin, Australia : implications for the duration of the intracratonic Petermann Orogeny /." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09SB/09sbw1191.pdf.
Повний текст джерелаWalsh, A. K. "Duration of the Petermann Orogeny from coupled diffusion and phase equilibria modelling." Thesis, 2010. http://hdl.handle.net/2440/106280.
Повний текст джерелаThe 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