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Статті в журналах з теми "Mount Painter Inlier"
Hore, S. B., S. M. Hill, and N. F. Alley. "Early Cretaceous glacial environment and paleosurface evolution within the Mount Painter Inlier, northern Flinders Ranges, South Australia." Australian Journal of Earth Sciences 67, no. 8 (April 15, 2020): 1117–60. http://dx.doi.org/10.1080/08120099.2020.1730963.
Повний текст джерелаBrugger, J., N. Meisser, B. Etschmann, S. Ansermet, and A. Pring. "Paulscherrerite from the Number 2 Workings, Mount Painter Inlier, Northern Flinders Ranges, South Australia: "Dehydrated schoepite" is a mineral after all." American Mineralogist 96, no. 2-3 (February 1, 2011): 229–40. http://dx.doi.org/10.2138/am.2011.3601.
Повний текст джерелаArmit, R. J., P. G. Betts, B. F. Schaefer, M. J. Pankhurst, and D. Giles. "Provenance of the Early Mesoproterozoic Radium Creek Group in the northern Mount Painter Inlier: Correlating isotopic signatures to inform tectonic reconstructions." Precambrian Research 243 (April 2014): 63–87. http://dx.doi.org/10.1016/j.precamres.2013.12.022.
Повний текст джерелаHore, S. B., S. M. Hill, A. Reid, B. Wade, N. F. Alley, and D. R. Mason. "U–Pb geochronology reveals evidence of a Late Devonian hydrothermal event, and protracted hydrothermal–epithermal system, within the Mount Painter Inlier, northern Flinders Ranges, South Australia." Australian Journal of Earth Sciences 67, no. 7 (August 19, 2020): 1009–44. http://dx.doi.org/10.1080/08120099.2020.1793383.
Повний текст джерелаДисертації з теми "Mount Painter Inlier"
Teasdale, Jonathan. "Proterozoic tectonic models with application to the Mount Painter inlier /." Title page and abstract only, 1993. http://web4.library.adelaide.edu.au/theses/09SB/09sbt253.pdf.
Повний текст джерелаSlade, John V. "Metamorphism of a northern segment of the Mount Painter Inlier, South Australia /." Adelaide, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbs631.pdf.
Повний текст джерелаWeisheit, Anett [Verfasser], and Paul [Akademischer Betreuer] Bons. "Structural and hydrothermal evolution of the Mount Painter Inlier, South Australia / Anett Weisheit ; Betreuer: Paul D. Bons." Tübingen : Universitätsbibliothek Tübingen, 2013. http://d-nb.info/1162844736/34.
Повний текст джерелаWeisheit, Anett Verfasser], and Paul [Akademischer Betreuer] [Bons. "Structural and hydrothermal evolution of the Mount Painter Inlier, South Australia / Anett Weisheit ; Betreuer: Paul D. Bons." Tübingen : Universitätsbibliothek Tübingen, 2013. http://d-nb.info/1162844736/34.
Повний текст джерелаNeumann, Narelle L. "Isotopic and geochemical characteristics of the British Empire granite as indicators of magma provenance and processes of melt generation in the Mount Painter Inlier, South Australia /." Title page, contents and abstract only, 1996. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bn492.pdf.
Повний текст джерелаNeumann, N. L. "Isotopic and geochemical characteristics of the British Empire Granite as indicators of magma provenance and processes of melt generation in the Mount Painter Inlier, South Australia." Thesis, 1996. http://hdl.handle.net/2440/114328.
Повний текст джерелаThe production of granitic magmas at shallow to midcrustal depths by anatexis of crustal material requires a significant thermal perturbation of the normal crustal geothermal regime. Thermal perturbations leading to anatexis may be initiated by crustal thickening associated with deformation, intrusion and/or upwelling of heat sources from lower crust or mantle regions or by anomalous concentrations of heat-producing elements, U, Th and K. This thesis explores the origin of shallow to mid-crustal peraluminous granites within the Mount Painter Inlier, together with their relationship to older granite suites, as indicators of magmatic processes during crustal deformation of the Delamerian Orogeny. The geochemical and isotopic characteristics of granites and gneisses of the Mount Painter Inlier indicate two distinct periods of granitic evolution involving different source regions and magmatic processes. Proterozoic granites and gneisses reflect magmatic sources and processes similar to those involved in the evolution of other Australian anorogenic Proterozoic terrains, although extreme concentrations of U, Th and K suggest an important role for element concentration within accessory minerals during granite genesis. Field relationships, together with geochemical and isotopic characteristics of the Palaeozoic(?) British Empire Granite indicate evolution from a complex mixture of surrounding metasediments and granites in a number of possible scenarios. The additional thermal energy required to produce the British Empire Granite from partial melting of this package at depths of approximately 12 to 15 km is consistent with perturbed thermal regimes resulting from anomalous internal heat production due to the extreme concentration of U, Th and K within the Proterozoic units.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1996
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.
Повний текст джерелаIncludes 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
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.
Повний текст джерелаIncludes 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
Johnson, A. K. "Biogeochemical expression of uranium mineralisation and geology, by Eucalyptus camaldulensis in the Paralana Creek drainage system, South Australia." Thesis, 2009. http://hdl.handle.net/2440/128961.
Повний текст джерелаMineral exploration in Australia today faces a great challenge: to efficiently detect mineralisation buried beneath extensive regolith cover. Because their roots penetrate the regolith cover, establishing the elemental signatures of certain plants (biogeochemical exploration) can aid in the detection of buried ore deposits. At the highly prospective Mount Painter Inlier, Eucalyptus camaldulensis (river red gum) was sampled in the ranges and extending out onto the plains bordering Lake Frome. Here it is shown that the leaves from Eucalyptus trees can detect a range of elements including important pathfinder elements related to U mineralisation. A significant finding of this study is that the sediments thought to be associated with the geochemical transport and host of U mineralisation, like those that host the Four Mile U deposit, have relatively elevated U2/Th values. The geological setting of these locally elevated U results also appears to be equivalent to the Four Mile mineralisation, based on available field exposures. Therefore, this area could well represent a biogeochemical expression of mineralisation equivalent to the soon to be mined Four Mile U deposit. This study demonstrated that Eucalyptus biogeochemistry has significant advantages over other approaches in that it is cost and time efficient, culturally unobtrusive, and can identify relationships between plant biogeochemistry and the underlying geological substrate, in particular, U-mineralisation. The examination of more Eucalyptus camaldulensis (and more widespread species in the area) from surrounding areas therefore also warrants further investigation.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2009