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Статті в журналах з теми "Mount Painter Province"
Armit, R. J., P. G. Betts, B. F. Schaefer, and L. Ailleres. "Constraints on long-lived Mesoproterozoic and Palaeozoic deformational events and crustal architecture in the northern Mount Painter Province, Australia." Gondwana Research 22, no. 1 (July 2012): 207–26. http://dx.doi.org/10.1016/j.gr.2011.11.003.
Повний текст джерелаMcLAREN, SANDRA, MIKE SANDIFORD, ROGER POWELL, NARELLE NEUMANN, and JON WOODHEAD. "Palaeozoic Intraplate Crustal Anatexis in the Mount Painter Province, South Australia: Timing, Thermal Budgets and the Role of Crustal Heat Production." Journal of Petrology 47, no. 12 (September 8, 2006): 2281–302. http://dx.doi.org/10.1093/petrology/egl044.
Повний текст джерелаArmit, R. J., L. Ailleres, P. G. Betts, B. F. Schaefer, and T. N. Blaikie. "High-heat geodynamic setting during the Palaeozoic evolution of the Mount Painter Province, SA, Australia: evidence from combined field structural geology and potential-field inversions." Geophysical Journal International 199, no. 1 (August 7, 2014): 253–75. http://dx.doi.org/10.1093/gji/ggu263.
Повний текст джерелаHouston, Walter J. "Between Salem and Mount Gerizim: The Context of the Formation of the Torah Reconsidered." Journal of Ancient Judaism 5, no. 3 (May 14, 2014): 311–34. http://dx.doi.org/10.30965/21967954-00503003.
Повний текст джерелаGeorges, Arthur, Erika Alacs, Matthew Pauza, Felix Kinginapi, Amos Ona, and Carla Eisemberg. "Freshwater turtles of the Kikori Drainage, Papua New Guinea, with special reference to the pig-nosed turtle, Carettochelys insculpta." Wildlife Research 35, no. 7 (2008): 700. http://dx.doi.org/10.1071/wr07120.
Повний текст джерелаSpehar, Perica, Natasa Miladinovic-Radmilovic, and Sonja Stamenkovic. "Late antique necropolis in Davidovac-Crkviste." Starinar, no. 63 (2013): 269–86. http://dx.doi.org/10.2298/sta1363269s.
Повний текст джерела"A mural tomb of the Northern Dynasties at Jiuyuangang in Xinzhou City, Shanxi Province." Chinese Archaeology 16, no. 1 (November 27, 2016): 49–67. http://dx.doi.org/10.1515/char-2016-0004.
Повний текст джерелаДисертації з теми "Mount Painter Province"
Smith, Peter B. "The alteration history of late Proterozoic Wooltana volcanics, Mount Painter Province, S.A. /." Adelaide, 1992. http://web4.library.adelaide.edu.au/theses/09SB/09sbs656.pdf.
Повний текст джерелаNational grid reference SH54 - 6737-2. One coloured folded map in pocket inside back pocket. Includes bibliographical references.
Godsmark, Bruce Nye. "Metamorphism and hydrothermal history of the Yudnamutana Copper Field, Mount Painter province, South Australia /." Title page, table of contents and abstract only, 1993. http://web4.library.adelaide.edu.au/theses/09SB/09sbg589.pdf.
Повний текст джерелаNational grid reference: Yudnamutana sheet (SH-54) 6737 I. Includes bibliographical references (leaves 22-24).
Smith, Andrea B. "Geology of the Yudnamutana Gorge, Paralana Hot Springs area and genesis of mineralization at the Hodgkinson prospect, Mount Painter Province, South Australia /." Adelaide, 1992. http://web4.library.adelaide.edu.au/theses/09SB/09sbs642.pdf.
Повний текст джерелаTwo coloured folded maps in pocket inside back cover. "National grid reference (S1-54) 6737-1." Includes bibliographical references (leaves [8-10]).
Smith, P. B. "The alteration history of Late Proterozoic Wooltana Volcanics, Mount Painter Province, S.A." Thesis, 1992. http://hdl.handle.net/2440/131151.
Повний текст джерелаThe Wooltana Volcanics experienced a pervasive low grade hydrothermal alteration prior to the Delamerian. The timing of this event is poorly constrained. However the available evidence is consistent with the metasomatism occurring during the active stretching thought to have caused the uplift related refrigeration responsible for the formation of the Merinjina Tillite. This study confirms the proposals of previous workers that the Wooltana Volcanics, Beda Volcanics and Gairdner Dyke Swarm are temporal equivalents, although this study has shown the Gairdner Dyke Swann to be a systematically fractionated end member. The Wooltana Volcanics are very like the Parana low-Ti CFB of Brazil and also the dolerites from the Atlas Mountains of Morocco. Both are associated with magmatic events immediately preceding the first openings of the Atlantic Ocean. The occurrence of the Port Pirie Volcanics within Burra Group sediments suggests a reoccurrence of mantle decompression due to lithospheric stretching further to the south.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1992
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
Job, A. L. "Evolution of the basal Adelaidean in the northern Flinders Ranges: deposition, provenance and deformation of the Callanna and lower Burra Groups." Thesis, 2011. http://hdl.handle.net/2440/96175.
Повний текст джерелаThe rift and deformational evolution of the Adelaide Fold Belt’s northern-most extent, the northern Flinders Ranges, has received comparatively little attention than that of the southern Adelaide Fold Belt. The Arkaroola area, located in the mid-north northern Flinders Ranges, exposes the lowermost Adelaidean stratigraphy of this rift complex, the Callanna and lower Burra Groups, in a near complete sedimentary sequence. The rift history of this stratigraphy is complex, with deposition being largely controlled by the northeast-southwest orientated Paralana Fault and similarly orientated local growth faults. Locally, the Paralana Fault deviates from its regional orientation and forms a north-south striking segment, which under a considered sinistral strike-slip regime during extension would potentially create localised transtension in a ‘releasing bend’ environment. Rifting in the Arkaroola area is therefore considered to be analogous to the formation of a pull-apart basin. U-Pb dating of detrital zircons from the Paralana Quartzite, Humanity Seat Formation and Blue Mine Conglomerate from the Callanna and lower Burra groups yields ages that are comparable to local source regions the Gawler Craton, Mount Painter Basement Complex and the Curnamona Province, and suggest proximal derivation during early rift phases. Sm-Nd bulk rock analysis on the finer grained Woodnamoka Formation implies derivation from the Mount Painter Basement Complex or the upper Willyama Supergroup of the Curnamona Province, the latter of which potentially suggests a more distal provenance region outside of the Australian continent. Deformation in the northern Flinders Ranges has previously been largely ascribed to the ca. 500 Ma Delamerian Orogeny. However, the Arkaroola area exhibits complex deformation not observed in the directly overlying gently folded stratigraphy. Reactivation of pull-apart rift structures during transpression is considered a possible mechanism for producing and localising such deformation. The possibility of an early Neoproterozoic deformational event occurring prior to deposition of the lesser-deformed overlying stratigraphy is also considered, but in lieu of an unequivocal orogenic unconformity, cannot be confidently ascribed. Temporal constraints defined by this study are too broad to accurately define the timing of deformation, and therefore its timing and potential relationship to the Delamerian Orogeny remains largely enigmatic.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011