Добірка наукової літератури з теми "Alice Springs Orogeny"
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Статті в журналах з теми "Alice Springs Orogeny"
Moussavi-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 джерелаRoberts, Emily A., and Gregory A. Houseman. "Geodynamics of central Australia during the intraplate Alice Springs Orogeny: thin viscous sheet models." Geological Society, London, Special Publications 184, no. 1 (2001): 139–64. http://dx.doi.org/10.1144/gsl.sp.2001.184.01.08.
Повний текст джерелаBradshaw, J. D., and P. R. Evans. "PALAEOZOIC TECTONICS, AMADEUS BASIN, CENTRAL AUSTRALIA." APPEA Journal 28, no. 1 (1988): 267. http://dx.doi.org/10.1071/aj87021.
Повний текст джерелаGibson, H. J., G. Ambrose, I. R. Duddy, P. R. Tingate, and T. Marshall. "POST–EARLY CARBONIFEROUS THERMAL HISTORY RECONSTRUCTION FROM WELL DATA IN THE AMADEUS BASIN, CENTRAL AUSTRALIA." APPEA Journal 44, no. 1 (2004): 357. http://dx.doi.org/10.1071/aj03013.
Повний текст джерелаBUICK, I. S., A. STORKEY, and I. S. WILLIAMS. "Timing relationships between pegmatite emplacement, metamorphism and deformation during the intra-plate Alice Springs Orogeny, central Australia." Journal of Metamorphic Geology 26, no. 9 (December 2008): 915–36. http://dx.doi.org/10.1111/j.1525-1314.2008.00794.x.
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 джерелаRaimondo, Tom, Martin Hand, Chris Clark, Kevin Faure, and Alan S. Collins. "Sources, thermal conditions and mechanisms of fluid ingress during regional rehydration of Alice Springs Orogeny intracratonic shear systems." Journal of Geochemical Exploration 101, no. 1 (April 2009): 84. http://dx.doi.org/10.1016/j.gexplo.2008.11.008.
Повний текст джерелаAmbrose, G. J., P. D. Kruse, and P. E. Putnam. "GEOLOGY AND HYDROCARBON POTENTIAL OF THE SOUTHERN GEORGINA BASIN, AUSTRALIA." APPEA Journal 41, no. 1 (2001): 139. http://dx.doi.org/10.1071/aj00007.
Повний текст джерелаQuentin de Gromard, Raphael. "The significance of E–W structural trends for the Alice Springs Orogeny in the Charters Towers Province, North Queensland." Tectonophysics 587 (March 2013): 168–87. http://dx.doi.org/10.1016/j.tecto.2012.09.002.
Повний текст джерелаPhillips, Bruce J., Alan W. James, and Graeme M. Philip. "THE GEOLOGY AND HYDROCARBON POTENTIAL OF THE NORTH-WESTERN OFFICER BASIN." APPEA Journal 25, no. 1 (1985): 52. http://dx.doi.org/10.1071/aj84004.
Повний текст джерелаДисертації з теми "Alice Springs Orogeny"
Haddow, D. J. "Structural and geochronological constraints on the origin and evolution of rocks in the Ormiston Pound region of the Western MacDonnell Ranges, Northern Territory." Thesis, 2009. http://hdl.handle.net/2440/128940.
Повний текст джерелаThe Arunta Inlier preserves a complex structural history, subject to a series of igneous, metamorphic and deformational events from the Paleoproterozoic to the mid-Paleozoic. U-Pb detrital zircon ages from Paleoproterozoic and Neoproterozoic sediments at Ormiston Gorge coincide with the timing of various tectonic phases in the Arunta Inlier. First order interpretations suggest that the Northern Arunta Inlier was the source of the oldest zircons recorded at ~1820 Ma, coinciding with the timing of the Stafford Event. The Strangways Orogeny at ~1770 Ma and 1730 Ma is the earliest deformation preserved in the Central Arunta Inlier and is probably the source of zircons accumulated in these sediments. Zircons post-dating the Strangways Orogeny are likely sourced from the Southern Arunta Inlier, coinciding with the Argilke Tectonic Event at ~1680 Ma, the Chewings Orogeny at ~1600 Ma, the Anmatjira Uplift Phase at 1500-1400 Ma and the emplacement of the Teapot Granite Complex at ~1140 Ma. The Neoproterozoic Heavitree Range Quartzite sediments represent initial deposition in the Amadeus Basin, which forms the remnant of a once much larger intracratonic basin in central Australia known as the Centralian Superbasin. The Arunta Inlier was exhumed from beneath the Centralian Superbasin during the Devonian-Carboniferous Alice Springs Orogeny, forming a series of subbasins including the Amadeus, Ngalia and Georgina Basins. North-south crustal compression during this Orogeny reactivated a series of steep north-dipping Mesoproterozoic fault structures including the Redbank shear zone and the Ormiston thrust zone. The northern Amadeus Basin is characterised by coupled basement and cover deformation, producing a series of basement-rooted south-propagating thrusts, which penetrate the basal Heavitree Range Quartzite. Structural cross-sections constructed across the Ormiston region propose a series of splay thrusts within the Ormiston thrust zone, with the basement and Heavitree Quartzite heavily deformed. The conformably overlying Bittersprings Formation comprises salts and evaporates, interpreted as a detachment layer. 40Ar/39Ar muscovite dating of mylonitic shear zones at Ormiston Gorge have constrained ‘peak deformation’ conditions in the region to a minimum age of 350 ± 3 Ma. Mineral assemblages formed in the surrounding areas reflect greenschist to lower amphibolite facies metamorphism, with temperatures reaching at least 350°C.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, YEAR
Pointon, V. J. "Structure and thermochronology of an E-W profile through the Mount Painter Province, Northern Flinders Ranges, South Australia: is this a southern example of deformation and exhumation driven by the Alice Springs Orogeny?" Thesis, 2010. http://hdl.handle.net/2440/88635.
Повний текст джерелаThe Mount Painter Province in the Northern Flinders Ranges, South Australia is composed of Palaeoproterozoic to Mesoproterozoic basement overlain by 7-12 kilometres of Neoproterozoic to Cambrian sedimentary rocks and is associated with high lateral geothermal gradients. During the Early Paleozoic, deformation and metamorphism reached greenschist to amphibolite facies during the ~500 Ma Delamerian Orogeny. This study focuses on the subsequent thermal history of the area by studying an E-W profile through the Mount Painter Province using the widely used techniques of structural mapping, micro-structural analysis and 40Ar/39Ar thermochronology to characterise and date deformation and cooling (as a proxy for exhumation). The E-W trending profile, known as the Hamilton Fault, is south dipping oblique slip with a normal and dextral component overprinted by younger brittle structures and brecciation which is seen in the structural and micro-structural analysis.. It is proposed to have a very active past and there is evidence of movement in the Adelaidean due to an apparent formation offset of ~600 m. The regional context of the Hamilton Fault having a dextral and normal component suggests an ε3 uplift, an ε2 extension SW to NE and ε1 NW-SE shortening. This is similar in character to the N-S shortening which is seen in the Alice Springs Orogeny (ASO). Results from the 40Ar/39Ar thermochronology show the basement metasedimentary rocks have cooling ages of around ~350 Ma between 300 to 400 °C and 312 Ma at 150 °C. Interestingly, the younger Adelaidean metasedimentary rocks have an older cooling age of 390 Ma between 300 to 400 °C. The thermochronology data suggests differential cooling has occurred. The observations suggest that exhumation is driven following the Delamerian folding event and forced the earlier cooling of shallower samples at a slower rate and later cooling of the deeper samples at a faster rate, a process caused by differential tilting. The cooling paths are well represented in this example as shown by converging cooling paths. Overall I attribute this subsequent thermal history and structural similarity to the ASO, a major widespread dramatic orogenic event which has not been widely recognized as a significant tectonic event in the Adelaide Fold Belt.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2010