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Статті в журналах з теми "Structural Queensland Mount Isa Inlier"
O'dea, Mark G., and Gordon S. Lister. "The role of ductility contrast and basement architecture in the structural evolution of the Crystal Creek block, Mount Isa Inlier, NW Queensland, Australia." Journal of Structural Geology 17, no. 7 (July 1995): 949–60. http://dx.doi.org/10.1016/0191-8141(94)00117-i.
Повний текст джерелаHutton, Laurie, Melanie Fitzell, Kinta Hoffmann, Ian Withnall, Bernie Stockill, Ben Jupp, and Paul Donchak. "The Millungera Basin—new geoscience supporting exploration." APPEA Journal 50, no. 2 (2010): 727. http://dx.doi.org/10.1071/aj09091.
Повний текст джерелаPasschier, C. W., and P. R. Williams. "Proterozoic extensional deformation in the Mount Isa inlier, Queensland, Australia." Geological Magazine 126, no. 1 (January 1989): 43–53. http://dx.doi.org/10.1017/s0016756800006130.
Повний текст джерелаMcConachie, B. A., M. G. Barlow, J. N. Dunster, R. A. Meaney, and A. O. Schaap. "THE MOUNT ISA BASIN—DEFINITION, STRUCTURE AND PETROLEUM GEOLOGY." APPEA Journal 33, no. 1 (1993): 237. http://dx.doi.org/10.1071/aj92018.
Повний текст джерелаJayawardhana, Prasantha Michael, and S. N. Sheard. "The use of airborne gamma‐ray spectrometry—A case study from the Mount Isa inlier, northwest Queensland, Australia." GEOPHYSICS 65, no. 6 (November 2000): 1993–2000. http://dx.doi.org/10.1190/1.1444883.
Повний текст джерелаStumpfl, E. F. "Geology of the Mount Isa Inlier and Environs, Queensland and Northern Territory." Ore Geology Reviews 4, no. 3 (March 1989): 275–76. http://dx.doi.org/10.1016/0169-1368(89)90020-6.
Повний текст джерелаNeudert, Martin K. "Geology of the Mount Isa Inlier and Environs, Queensland and Northern Territory." Earth-Science Reviews 27, no. 3 (May 1990): 277–78. http://dx.doi.org/10.1016/0012-8252(90)90014-m.
Повний текст джерелаSalama, Walid, Michael F. Gazley, and Lindsay C. Bonnett. "Geochemical exploration for supergene copper oxide deposits, Mount Isa Inlier, NW Queensland, Australia." Journal of Geochemical Exploration 168 (September 2016): 72–102. http://dx.doi.org/10.1016/j.gexplo.2016.05.008.
Повний текст джерелаWilliams, Patrick J., and Maree Heinemann. "Maramungee; a Proterozoic Zn skarn in the Cloncurry District, Mount Isa Inlier, Queensland, Australia." Economic Geology 88, no. 5 (August 1, 1993): 1114–34. http://dx.doi.org/10.2113/gsecongeo.88.5.1114.
Повний текст джерелаLoosveld, Ramon J. H. "The intra-cratonic evolution of the central eastern Mount Isa Inlier, northwest Queensland, Australia." Precambrian Research 44, no. 3-4 (October 1989): 243–76. http://dx.doi.org/10.1016/0301-9268(89)90047-8.
Повний текст джерелаДисертації з теми "Structural Queensland Mount Isa Inlier"
Bruce, Matthew. "The structural setting of the Knapdale Quartzite, Mount Isa Inlier /." Title page, abstract and contents only, 1999. http://web4.library.adelaide.edu.au/theses/09SB/09sbb887.pdf.
Повний текст джерелаNational grid reference Quamby (6957) 1:100 000 sheet. One col. folded map in pocket pasted onto back cover. Includes bibliographical references (4 leaves).
McLaren, Sandra. "The role of internal heat production during metamorphism of the Eastern Arunta Complex, central Australia, and the Mount Isa Inlier, Queensland /." Title page, contents and abstract only, 1996. http://web4.library.adelaide.edu.au/theses/09SB/09sbm161.pdf.
Повний текст джерелаNational Grid reference SF53-14 (Alice Springs), SF54-1 (Mount Isa) (1:250 000). Includes bibliographical references (leaves [32-36]).
O'Brien, S. P. "Structural and mineralogical controls on the formation of the ‘Inter-lens’ at the Ernest Henry Deposit, Queensland." Thesis, 2016. http://hdl.handle.net/2440/121125.
Повний текст джерелаThe Ernest Henry Iron-oxide Copper Gold (IOCG) deposit is by far the largest in the Eastern Succession of the Mount Isa Inlier. In the current genetic model, the release of CO2 from fluids sourced from enriched mantle was critical to brecciation and mineralisation. However, a weakly mineralised and brecciated shear zone within the orebody named the ‘Inter-lens’ separates the orebody into two distinct lenses. The Inter-lens was not well reported early in the life of the mine and has not been taken into account in the current ore deposit models. Establishing the relative timing of the Inter-lens structure provides strong geological constraints for the formation of the orebody. In this study, optical petrographic investigations, Scanning Electron Microscopy (SEM) and Mineral Liberation Analysis (MLA) were used to investigate the protolith. Key mineral relationships and textures were assessed to reveal the paragenesis of the Inter-lens. Structural observations in oriented drill core complemented underground mapping of exposures of the Inter-lens to reveal the deformational history of the Inter-lens with respect to the Ernest Henry orebody. The protolith was revealed to be Mount Fort Constantine Metavolcanics that have undergone intense deformation with a metasomatic evolution broadly consistent with the main orebody. Mineralisation stages overprinted tectonic fabrics via veining, replacement and infill, providing direct evidence that the Inter-lens is a pre-mineralisation structure. Preservation of the Inter-lens during brecciation and mineralisation of the Ernest Henry deposit requires that the currently accepted ‘explosive’ breccia model must be revised.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2016
Loosveld, Ramon J. H. "Structure and tectono-thermal history of the Eastern Mount Isa Inlier, Australia." Phd thesis, 1988. http://hdl.handle.net/1885/140534.
Повний текст джерелаMurison, C. "Characteristics and ore genesis of the Mount Cuthbert deposit, Kalkadoon-Leichardt Belt, Mt Isa Inlier, north west Queensland." Thesis, 2015. http://hdl.handle.net/2440/118206.
Повний текст джерелаThe Mount Cuthbert mine is situated ~100km NE of Mt Isa near the eastern edge of the Kalkadoon Leichhardt Belt (KLB); a Proterozioc block of the Mt Isa Inlier that divides the world class mineral regions of the IOCG-style Eastern Fold Belt (EFB) and the Mount Isa style copper deposits of the Western Fold Belt (WFB). KLB hosted deposits display characteristics related to both the EFB and WFB style of mineralisation; however mineralisation at Mount Cuthbert is indicative of a genesis for KLB hosted deposits related to metasomatic and tectonic events responsible for mineralisation in the EFB. The Mount Cuthbert mine is a low tonnage-high grade, shear controlled, retrograde chalcopyrite-pyrite-pyrrhotite deposit hosted within silica-dolomite and biotite-chlorite altered schists and felsic volcanic units of the Leichhardt Volcanics. The paragenetic alteration sequence is composed of 5 alteration stages: Stage 1) sodic alteration (albite + quartz); Stage 2) K-Fe-Ca alteration (siderite + calcite + dolomite+ quartz + biotite ± magnetite ± ilmenite ± apatite ± pyrite); Stage 3) mineralisation (chalcopyrite + quartz ± pyrite ± pyrrhotite ± calcite ± chlorite); Stage 4) major chloritisation; Stage 5) oxidation and localised enrichment to chalcocite. The alteration halo within the deposit is characterised by a proximal alteration envelope (<50m) consisting of chalcopyrite, pyrite, quartz, dolomite and chlorite, an intermediate alteration envelope (50-500m) described by quartz-carbonate veining with minor chalcopyrite, pyrite and pyrrhotite, in addition to extensive biotite and chlorite alteration and minor magnetite alteration. A distal alteration envelope (>500m) is identified tentatively as albite dominant. The trace geochemistry of the main chalcopyrite ± pyrite ore phase reveals elevated Ni, Zn, Cd and Hg in pyrite and elevated Sn, Pb, Se, V, Cr, Te, Ga, As, Cd, Mo, Ga, Bi and Sb in chalcopyrite. Differing elemental trends within the ore minerals supports paragenetic evidence suggesting several phases of sulphide growth. The characteristics and features of the Mount Cuthbert deposit outlined in this study show the greatest number of similarities to other low tonnage-high grade, shear hosted deposits present in the KLB (i.e. Mighty Atom, Orphan). This suggests that despite having a genesis related to that of the EFB, KLB deposits are uniquely their own style of mineralisation. This supports a shear-zone associated exploration model that is specific to the KLB.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2015
Long, Ryan David. "The Paroo Fault and the Mount Isa copper orebodies; a revised structural and evolutionary model, Mt Isa, Queensland, Australia." Thesis, 2010. https://researchonline.jcu.edu.au/19039/1/01front.pdf.
Повний текст джерелаCreus, Pieter K. "3D structural controls of the shear zone hosted Dugald River zinc-lead-silver deposit, Mount Isa Inlier, Australia." Thesis, 2022. https://researchonline.jcu.edu.au/76653/1/JCU_76653_Creus_2022_thesis.pdf.
Повний текст джерелаMcLaren, 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
Davis, Toby Patrick. "Structural controls on Zn-Pb-Ag mineralisation determined by scale integrated analysis at Mount Isa, Queensland, Australia." Thesis, 2004. https://researchonline.jcu.edu.au/24945/1/01front-partsA-C.pdf.
Повний текст джерелаКниги з теми "Structural Queensland Mount Isa Inlier"
Geology of the Mount Isa Inlier and environs, Queensland and Northern Territory. Canberra: Australian Govt. Pub. Service, 1987.
Знайти повний текст джерелаHone, I. G. Physical property measurements on rock samples from the Mount Isa Inlier, northwest Queensland. Canberra: Australian Govt. Pub. Service, 1987.
Знайти повний текст джерелаJ, Stewart A., Blake, D. H., fl. 1967-, and Australia. Bureau of Mineral Resources, Geology and Geophysics., eds. Detailed studies of the Mount Isa inlier. Canberra: Australian Govt. Pub. Service, 1992.
Знайти повний текст джерелаТези доповідей конференцій з теми "Structural Queensland Mount Isa Inlier"
Horvath, Peter, and Jürgen Reinhardt. "LOW-PRESSURE, HIGH-TEMPERATURE METAPELITIC ROCKS FROM THE CENTRAL MOUNT ISA INLIER, NW QUEENSLAND, AUSTRALIA: NEW RESULTS FROM QUANTITATIVE PHASE DIAGRAM CALCULATIONS." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-380451.
Повний текст джерела