Academic literature on the topic 'Olary Domain'
Create a spot-on reference in APA, MLA, Chicago, Harvard, and other styles
Contents
Consult the lists of relevant articles, books, theses, conference reports, and other scholarly sources on the topic 'Olary Domain.'
Next to every source in the list of references, there is an 'Add to bibliography' button. Press on it, and we will generate automatically the bibliographic reference to the chosen work in the citation style you need: APA, MLA, Harvard, Chicago, Vancouver, etc.
You can also download the full text of the academic publication as pdf and read online its abstract whenever available in the metadata.
Journal articles on the topic "Olary Domain"
Law, Steve, and Stephen Busuttil. "Geophysics of the Kalkaroo prospect, Olary Domain, South Australia." ASEG Extended Abstracts 2003, no. 3 (December 2003): 121–26. http://dx.doi.org/10.1071/asegspec12_10.
Full textGriessmann, Martin, Andreas Schmidt Mumm, Thomas Seifert, and Colin Conor. "The Mt. Mulga barite–magnetite–copper–gold mineralisation, Olary Domain, South Australia." Journal of Geochemical Exploration 106, no. 1-3 (July 2010): 110–20. http://dx.doi.org/10.1016/j.gexplo.2009.11.008.
Full textPepper, M. A., and P. M. Ashley. "Volcanic textures in quartzo‐feldspathic gneiss of the Willyama Supergroup, Olary Domain, South Australia." Australian Journal of Earth Sciences 45, no. 6 (December 1998): 971–78. http://dx.doi.org/10.1080/08120099808728451.
Full textAshley, P. M., B. G. Lottermoser, and J. M. Westaway. "Iron-formations and epigenetic ironstones in the Palaeoproterozoic Willyama Supergroup, Olary Domain, South Australia." Mineralogy and Petrology 64, no. 1-4 (March 1998): 187–218. http://dx.doi.org/10.1007/bf01226569.
Full textClark, Christopher, and Patrick James. "Hydrothermal brecciation due to fluid pressure fluctuations: examples from the Olary Domain, South Australia." Tectonophysics 366, no. 3-4 (May 2003): 187–206. http://dx.doi.org/10.1016/s0040-1951(03)00095-7.
Full textHills, Q. G., P. G. Betts, and G. S. Lister. "Geophysical interpretation and modelling of the Olary Domain under cover: A hidden inverted rift system." Australian Journal of Earth Sciences 50, no. 4 (August 2003): 633–44. http://dx.doi.org/10.1046/j.1440-0952.2003.01017.x.
Full textGriessmann, Martin, Andreas Schmidt Mumm, Thomas Seifert, and Colin Conor. "The mineralising system of the Mt. Mulga barite–magnetite–Cu–Au mineralisation, Olary Domain, South Australia." Journal of Geochemical Exploration 101, no. 1 (April 2009): 44. http://dx.doi.org/10.1016/j.gexplo.2008.12.059.
Full textCLARK, C., A. SCHMIDT MUMM, and K. FAURE. "Timing and nature of fluid flow and alteration during Mesoproterozoic shear zone formation, Olary Domain, South Australia." Journal of Metamorphic Geology 23, no. 3 (April 2005): 147–64. http://dx.doi.org/10.1111/j.1525-1314.2005.00568.x.
Full textClark, Chris, Ben Grguric, and Andreas Schmidt Mumm. "Genetic implications of pyrite chemistry from the Palaeoproterozoic Olary Domain and overlying Neoproterozoic Adelaidean sequences, northeastern South Australia." Ore Geology Reviews 25, no. 3-4 (October 2004): 237–57. http://dx.doi.org/10.1016/j.oregeorev.2004.04.003.
Full textPage, R. W., C. H. H. Conor, B. P. J. Stevens, G. M. Gibson, W. V. Preiss, and P. N. Southgate. "Correlation of Olary and Broken Hill Domains, Curnamona Province:Possible Relationship to Mount Isa andOther North Australian Pb-Zn-Ag-Bearing Successions." Economic Geology 100, no. 4 (June 1, 2005): 663–76. http://dx.doi.org/10.2113/gsecongeo.100.4.663.
Full textDissertations / Theses on the topic "Olary Domain"
Clark, Christopher F. P. "Hydrothermal brecciation due to fluid pressure fluctuations : examples from the Olary Domain, South Australia /." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09SB/09sbc5923.pdf.
Full textTaylor, Ashley David. "Structural mapping adjacent to the 'Woman-in-White amphibolite' in the Olary Domain, South Australia /." Title page, abstract and table of contents only, 1999. http://web4.library.adelaide.edu.au/theses/09SB/09sbt238.pdf.
Full textClark, Jonathan. "Structural and metamorphic investigation of the Cathedral Rock-Drew Hill area, Olary Domain, South Australia /." Title page, table of contents and abstract only, 1999. http://web4.library.adelaide.edu.au/theses/09SB/09sbc5931.pdf.
Full textKernich, Amy Lenore. "Weathering, erosion and element mobilisation in a catchment at the Luxemburg Copper/Gold site, Olary domain, South Australia /." Title page, table of contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09ENVSH/09envshk398.pdf.
Full textPenhall, John Lachlan. "A fluid inclusion and sulphur isotope study of epigenetic copper mineralisation in the Bimbowrie area, Olary Domain, South Australia /." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09SB/09sbp399.pdf.
Full textBrett, Damien. "Structural, geochemical and isotopic investigation of granitoids within the central area of the eastern Weekeroo Inlier, Olary Domain, South Australia /." Title page, abstract and contents only, 1998. http://web4.library.adelaide.edu.au/theses/09SB/09sbb8448.pdf.
Full textLau, Ian Christopher. "Regolith-landform and mineralogical mapping of the White Dam Prospect, eastern Olary Domain, South Australia, using integrated remote sensing and spectral techniques." Title page, abstract and table of contents only, 2004. http://hdl.handle.net/2440/37972.
Full textThesis (Ph.D.)--School of Earth & Environmental Sciences, 2004.
Gill, Robert Michael. "A magnetotelluric profile across the Broken Hill and Olary Domains /." Title page, table of contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09SB/09sbg4756.pdf.
Full textGill, R. M. "A magnetotelluric profile across the Broken Hill and Olary Domains." Thesis, 2002. http://hdl.handle.net/2440/113040.
Full textSeventeen magnetotelluric survey sites were occupied across the Olary and Broken Hill Domains in the Curnamona Province, Australia. Two dimensional modelling along the magnetotelluric profile identifies the Broken Hill Domain as a zone of high electrical resistivity to a depth of 15km. Gravity modelling along a coincident profile has also shown the Broken Hill Domain to be significantly more dense than its surrounds. Seismic data have provided evidence of numerous faults and shear zones within the Pre-cambrian Broken Hill Domain basement, and is indicative of compression during the Delamarian Orogeny. It is proposed that the majority of crustal fluids were removed from these rocks by granulite facies metamorphism and tectonic compression. The boundary of the Olary Domain appears to be delineated by the Mundi Mundi Fault with an order of magnitude increase in resistivity on the Broken Hill side. The location of the Flinders Conductivity Anomaly was also observed and a number of conducting mechanisms considered, including crustal fluids and graphite films.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2002
Taylor, A. D. "Structural mapping adjacent to the “Woman-in-White” amphibolite in the Olary Domain, South Australia." Thesis, 1999. http://hdl.handle.net/2440/119337.
Full textA structural study of Palaeoproterozoic Willyama Supergroup rocks to the southeast of Old Boolcoomata approximately 20 kilometres north of Olary, South Australia, discloses a complex history of deformation. This includes an axial planar S1 schistosity and several intersecting locally developed subsequent planar fabrics. The main findings support previous unpublished company studies. Structural maps were produced at various scales in areas surrounding the ‘Woman-in-White’ amphibolite and all available observations were used to form a chronology of events and tectonic model for the geometric and kinematic evolution of the area. In a domain east of the 'Woman-in-White' amphibolite the S1 is parallel to the axial plane of a major isoclinal synform closing to the east. S2 is axial planar to tight to open class 2 and class 1c F2 folds that trend generally north to northeast. Regionally, and particularly in the vicinity of the 'Woman-in-White' amphibolite, a third deformation is very intensely developed generating two fabrics. The S3 schistosity is the axial planar fabric to tight to isoclinal F3 folds trending consistently east-west. The S3 fabric is also expressed as a crenulation of the S1 regional schistosity. These pre-Adelaidean structural elements are recognised as comprising the Olarian Deformation. Fold interference is present on all scales. Olarian deformation events two and three have given the flat lying western limb of the principal F1 synform a luniform, dome and basin morphology. Type 2 and type 3 interference patterns are the most common in the area mapped. The occurrence of the two interference patterns is due to the variable angle between OD2 and OD3 compressions, which is commonly approximately 40 in the west-southwest part of the mapped area. This work conforms closely in complexity to previous regional studies and has been supplemented by other new investigations of an important northeast-southwest trending shear zone corresponding to OD3, lying further to the north, and a geochemical investigation of the 'Woman-in-White' amphibolite indicating its probable mantle origin and possible emplacement before all deformations occurred.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1999