Academic literature on the topic 'Metamorphism (Geology) South Australia Lofty'

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Journal articles on the topic "Metamorphism (Geology) South Australia Lofty"

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CLARKE, G. L., R. POWELL, and R. H. VERNON. "Reaction relationships during retrograde metamorphism at Olary, South Australia." Journal of Metamorphic Geology 13, no. 6 (November 1995): 715–26. http://dx.doi.org/10.1111/j.1525-1314.1995.tb00254.x.

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Sandiford, M., G. Eraser, J. Arnold, J. Foden, and T. Farrow. "Some causes and consequences of high‐temperature, low‐pressure metamorphism in the eastern Mt Lofty Ranges, South Australia." Australian Journal of Earth Sciences 42, no. 3 (June 1995): 233–40. http://dx.doi.org/10.1080/08120099508728197.

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Cartwright, Ian, Julie Vry, and Michael Sandiford. "Changes in stable isotope ratios of metapelites and marbles during regional metamorphism, Mount Lofty Ranges, South Australia: implications for crustal scale fluid flow." Contributions to Mineralogy and Petrology 120, no. 3-4 (July 1995): 292–310. http://dx.doi.org/10.1007/bf00306509.

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Cartwright, I., Julie Vry, and Michael Sandiford. "Changes in stable isotope ratios of metapelites and marbles during regional metamorphism, Mount Lofty Ranges, South Australia: implications for crustal scale fluid flow." Contributions to Mineralogy and Petrology 120, no. 3-4 (July 31, 1995): 292–310. http://dx.doi.org/10.1007/s004100050076.

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CLARKE, G. L., M. GUIRAUD, R. POWELL, and J. P. BURG. "Metamorphism in the Olary Block, South Australia: compression with cooling in a Proterozoic fold belt." Journal of Metamorphic Geology 5, no. 3 (July 1987): 291–306. http://dx.doi.org/10.1111/j.1525-1314.1987.tb00386.x.

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Twidale, C. Rowland. "Paul S. Hossfeld and His Contribution to Geomorphology." Historical Records of Australian Science 23, no. 2 (2012): 132. http://dx.doi.org/10.1071/hr12006.

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The received wisdom was and is that landscapes cannot be more than a few millions of years old. Nevertheless, consideration of local geology and age of sediments in adjacent basins convinced Paul S. Hossfeld that the summit surface of low relief preserved on the northern Mount Lofty Ranges of South Australia resulted from long-continued planation and that it is of Cretaceous age; that is, some 70 million years old. Hossfeld's apparently intuitive suggestion that very old landscapes exist, recorded in his graduate thesis but not further pursued by him, is the earliest known statement of this idea.
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Ward, Colin R., Peter R. Warbrooke, and F. Ivor Roberts. "Geochemical and mineralogical changes in a coal seam due to contact metamorphism, Sydney Basin, New South Wales, Australia." International Journal of Coal Geology 11, no. 2 (March 1989): 105–25. http://dx.doi.org/10.1016/0166-5162(89)90001-3.

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De Vries Van Leeuwen, Alexander T., Laura J. Morrissey, Tom Raimondo, and Martin Hand. "Prolonged high thermal gradient metamorphism in the Curnamona Province, south-central Australia, during the latter stages of Nuna assembly." Precambrian Research 378 (August 2022): 106775. http://dx.doi.org/10.1016/j.precamres.2022.106775.

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Halpin, Jacqueline A., and Anthony J. Reid. "Earliest Paleoproterozoic high-grade metamorphism and orogenesis in the Gawler Craton, South Australia: The southern cousin in the Rae family?" Precambrian Research 276 (May 2016): 123–44. http://dx.doi.org/10.1016/j.precamres.2016.02.001.

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Conn, C. Dakota, Paul G. Spry, Dan Layton-Matthews, Alexandre Voinot, and Alan Koenig. "The effects of amphibolite facies metamorphism on the trace element composition of pyrite and pyrrhotite in the Cambrian Nairne Pyrite Member, Kanmantoo Group, South Australia." Ore Geology Reviews 114 (November 2019): 103128. http://dx.doi.org/10.1016/j.oregeorev.2019.103128.

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Dissertations / Theses on the topic "Metamorphism (Geology) South Australia Lofty"

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Yassaghi, Ali. "Geometry, kinematics, microstructure, strain analysis, and P-T conditions of the shear zones and associated ductile thrusts in the southern Mt. Lofty Ranges/Adelaide Hills area, South Australia /." Title page, contents and abstract only, 1998. http://web4.library.adelaide.edu.au/theses/09PH/09phy29.pdf.

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Stevenson, Ross Kelley. "Implications of amazonite to sulfide-silicate equilibria." Thesis, McGill University, 1985. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63377.

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Tokarev, Victor. "Neotectonics of the Mount Lofty Ranges (South Australia) / Victor Tokarev." 2005. http://hdl.handle.net/2440/22225.

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"February, 2005"
Bibliography: leaves 259-272.
ix, 272 leaves : ill. (some col.), maps (col.), plates (col.) ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
"The Mount Lofty Ranges and flanking St Vincent and Western Murray Basins preserve a rich record of Australian intraplate neotectonic movements and their effects of landscape evolution and sedimentary basin development in this region of South Australia." "The major goal of this study is to develop a new tectonic model that contributes to our fundamental understanding of how neotectonic motions and deformations operate within this sector of the southern Australian Earth crust. The other main aim of this thesis is to provide a better understanding of the effects those neotectonic movements imposed on landscape evolution and sedimentation." --Introd.
Thesis (Ph.D.)--University of Adelaide, Faculty of Science, School of Earth and Environmental Sciences, Discipline of Geology and Geophysics, 2005
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Schiller, Jeffrey Christopher. "Structural geology, metamorphism and origin of the Kanmantoo Copper deposit, South Australia." Thesis, 2000. http://hdl.handle.net/2440/19902.

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Appendices 5 and 6 are made available in CD-ROM format (See 04SuppMaterial).
Includes copies of articles co-authored by the author during the preparation of this thesis as appendix 7.
14 maps (some folded, some col.); inserted in back pocket.
Includes bibliographical references (leaves 242-264).
System requirements for accompanying CD-ROM: Macintosh of IBM compatible computer. Other requirements: Adobe Acrobat Reader.
[15], 264 leaves : ill. (some col.), maps ; 30 cm. + 1 computer optical disk (4 3/4 in.)
On the basis of the present study it is concluded that there is no firm evidence that the bulk of the mineralisation is pre-metamorphic, although the possibility has not been excluded.
Thesis (Ph.D.) -- University of Adelaide, Dept. of Geology and Geophysics, 2001
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Schiller, Jeffrey Christopher. "Structural geology, metamorphism and origin of the Kanmantoo Copper deposit, South Australia / by Jeffrey Christopher Schiller." 2000. http://hdl.handle.net/2440/19902.

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Abstract:
Appendices 5 and 6 are made available in CD-ROM format.
Includes copies of articles co-authored by the author during the preparation of this thesis as appendix 7.
14 maps (some folded, some col.); inserted in back pocket.
Includes bibliographical references (leaves 242-264).
System requirements for accompanying CD-ROM: Macintosh of IBM compatible computer. Other requirements: Adobe Acrobat Reader.
[15], 264 leaves : ill. (some col.), maps ; 30 cm. + 1 computer optical disk (4 3/4 in.)
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
On the basis of the present study it is concluded that there is no firm evidence that the bulk of the mineralisation is pre-metamorphic, although the possibility has not been excluded.
Thesis (Ph.D.)--Adelaide University, Dept. of Geology and Geophysics, 2001
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Rutherford, Lachlan Stuart. "Developing a tectonic framework for the Southern Curnamona Cu - Au Province : geochemical and radiogenic isotope applications." 2006. http://hdl.handle.net/2440/37818.

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"Two independent geochronological techniques specifically targeting post-kinematic or late-stage growth of kyanite, staurolite and late-stage garnet in the southern Curnamona Province has found that these minerals grew during the Delamerian Orogeny (~530-500 Ma). Prograde metamorphism during the Delamerian Orogeny attained kyanite-staurolite-garnet grade (amphibolite-facies). Previous interpretations of an anticlockwise P-T path for the Olarian Orogeny need revising, as these interpretations have been shown in this study to be based on textural relationships spanning ~1100 million years. This highlights the importance of in situ geochronological techniques in defining robust P-T-t paths for a region." --p. 121 of source document.
Thesis (Ph.D.)--School of Earth and Environmental Sciences, 2006.
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Crowhurst, P. V. "The geology, petrology and geochemistry of the Proterozoic inlier, south of Myponga, Fleurieu Peninsula, South Australia." Thesis, 1988. http://hdl.handle.net/2440/119710.

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This item is only available electronically.
The study area is located within the Yankalilla-Myponga Proterozoic lnlier, approximately 60km south of Adelaide. The basement rocks are comprised of a mixture of metasediments and intrusives. The metasediments predominantly comprise of quartz-biotite gneisses and schists. They are intruded by basic dykes, pegmatites and an aplite/microgranite. The basic dykes have oceanic basalt affinities and could originally have been formed during an 'aborted rifting' event, but the more felsic rocks are more likely to lie within plate granites. The origin of the 'Houghton' granulite is difficult to ascertain, because it has a varied internal composition and is closely comparable to a diorite and a shale. The basement inlier rocks are found within the overlying unconformable upper Proterozoic Adelaidean System. They have undergone at least four phases of deformation and metamorphism. Mineral assemblages found in the rocks indicate metamorphism reached at least upper amphibolite facies. The maximum pressure and temperature conditions were calculated from microprobe data. They range from 8-10 kb at 550 -650 C. U-Pb isochron dating was performed on the aplite/microgranite of the area and was found to be 1578+\-22Ma ,which places a minimum age on the inlier rocks. This date obtained and the deformation processes recognized are comparable to other basement rocks in South Australia; noticeably the Gaw1er Craton and the Olary Province. This may indicate a homogeneous terrain once spanned most of South Australia during the lower Proterozoic.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1988
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Bollenhagen, W. J. "The influence of bulk rock MnO on garnet development in metamorphic rocks of andalusite-staurolite grade; Kanmantoo, South Australia." Thesis, 1993. http://hdl.handle.net/2440/109466.

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This item is only available electronically.
An outcrop of meta-pelitic schist from near the township of Kanmantoo, South Australia, was chosen to demonstrate the effect that increased bulk MnO content has on metamorphic assemblage development. From bulk composition and petrological analyses it is observed that the presence of small amounts of MnO in high XFe pelitic rocks correspond with the development of garnet. The incorporation of Mn into the KFMASH model system describes the existence of garnet with andalusite and staurolite that KFMASH does not predict. Furthermore it is shown that modal abundances of garnet are proportional to bulk MnO rock contents, enhancing the prediction that MnO causes an expansion of all garnet-bearing assemblages. This allows for the description of the numerous appearances of the garnet mineral in rocks that have calculated temperatures and pressures, for which it is not predicted to exist at.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1993
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9

McLaren, Sandra N. (Sandra Noeline). "Long-term consequences of the redistribution of heat producing elements within the continental crust: Australian examples / Sandra N. McLaren." 2001. http://hdl.handle.net/2440/19839.

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Includes copies of articles co-authored by author during the preparation of this thesis in back pocket.
Includes bibliographical references (leaves 113-124).
viii, 172 leaves : ill. (some col.), maps ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
Focuses on the impact of change in the distribution of heat producing elements on lithospheric thermal regimes and on temperature dependent processes such as metamorphism, magmatism and deformation, with application to Proteozoic Australia (Mount Isa and Mount Painter inliers).
Thesis (Ph.D.)--Adelaide University, Dept. of Geology and Geophysics, 2001
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McLaren, Sandra N. (Sandra Noeline). "Long-term consequences of the redistribution of heat producing elements within the continental crust: Australian examples / Sandra N. McLaren." Thesis, 2001. http://hdl.handle.net/2440/19839.

Full text
Abstract:
Includes copies of articles co-authored by author during the preparation of this thesis in back pocket.
Includes bibliographical references (leaves 113-124).
viii, 172 leaves : ill. (some col.), maps ; 30 cm.
Focuses on the impact of change in the distribution of heat producing elements on lithospheric thermal regimes and on temperature dependent processes such as metamorphism, magmatism and deformation, with application to Proteozoic Australia (Mount Isa and Mount Painter inliers).
Thesis (Ph.D.)--Adelaide University, Dept. of Geology and Geophysics, 2001
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