Добірка наукової літератури з теми "Central Gawler Craton"
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Статті в журналах з теми "Central Gawler Craton"
Hoatson, D. M., S. S. Sun, M. B. Duggan, M. B. Davies, S. J. Daly, and A. C. Purvis. "Late Archean Lake Harris Komatiite, Central Gawler Craton, South Australia:Geologic Setting and Geochemistry." Economic Geology 100, no. 2 (March 1, 2005): 349–74. http://dx.doi.org/10.2113/gsecongeo.100.2.349.
Повний текст джерелаHoatson, D. M. "Late Archean Lake Harris Komatiite, Central Gawler Craton, South Australia: Geologic Setting and Geochemistry." Economic Geology 100, no. 2 (March 1, 2005): 349–74. http://dx.doi.org/10.2113/100.2.349.
Повний текст джерелаFraser, G. L., R. G. Skirrow, A. Schmidt-Mumm, and O. Holm. "Mesoproterozoic Gold in the Central Gawler Craton, South Australia: Geology, Alteration, Fluids, and Timing." Economic Geology 102, no. 8 (December 1, 2007): 1511–39. http://dx.doi.org/10.2113/gsecongeo.102.8.1511.
Повний текст джерелаReid, Anthony, Richard Flint, Roland Maas, Katherine Howard, and Elena Belousova. "Geochronological and isotopic constraints on Palaeoproterozoic skarn base metal mineralisation in the central Gawler Craton, South Australia." Ore Geology Reviews 36, no. 4 (December 2009): 350–62. http://dx.doi.org/10.1016/j.oregeorev.2009.09.001.
Повний текст джерелаvan der Hoek, B. G., S. M. Hill, and Robert C. Dart. "Calcrete and plant inter-relationships for the expression of concealed mineralization at the Tunkillia gold prospect, central Gawler Craton, Australia." Geochemistry: Exploration, Environment, Analysis 12, no. 4 (November 2012): 361–72. http://dx.doi.org/10.1144/geochem2011-115.
Повний текст джерелаKelka, Ulrich, Cericia Martinez, Carmen Krapf, Stefan Westerlund, Ignacio Gonzalez-Alvarez, Mark Pawley, and Clive Foss. "Establishing an integrated workflow identifying and linking surface and subsurface lineaments for mineral exploration under cover: example from the Gawler Craton, South Australia." Solid Earth 13, no. 4 (April 29, 2022): 827–47. http://dx.doi.org/10.5194/se-13-827-2022.
Повний текст джерелаBoone, S. C., C. Seiler, A. J. Reid, B. Kohn, and A. Gleadow. "An Upper Cretaceous paleo-aquifer system in the Eromanga Basin of the central Gawler Craton, South Australia: evidence from apatite fission track thermochronology." Australian Journal of Earth Sciences 63, no. 3 (April 2, 2016): 315–31. http://dx.doi.org/10.1080/08120099.2016.1199050.
Повний текст джерелаCourtney-Davies, Liam, Cristiana L. Ciobanu, Nigel J. Cook, Max R. Verdugo-Ihl, Ashley Slattery, Sarah E. Gilbert, and Kathy Ehrig. "Metallic-Pb nanospheres in zircon from the Challenger Au deposit, South Australia: probing metamorphic and ore formation histories." Mineralogical Magazine 85, no. 6 (November 2, 2021): 868–78. http://dx.doi.org/10.1180/mgm.2021.81.
Повний текст джерелаHoward, K. E., M. Hand, K. M. Barovich, and E. Belousova. "Provenance of late Paleoproterozoic cover sequences in the central Gawler Craton: exploring stratigraphic correlations in eastern Proterozoic Australia using detrital zircon ages, Hf and Nd isotopic data." Australian Journal of Earth Sciences 58, no. 5 (July 2011): 475–500. http://dx.doi.org/10.1080/08120099.2011.577753.
Повний текст джерелаДисертації з теми "Central Gawler Craton"
Swain, Greg Martin. "Provenance and tectonics of the late Archaean mulgathing complex, central Gawler Craton : geochronological, geochemical and isotopic evidence for plume-arc interaction /." Title page, table of contents and abstract only, 2002. http://web4.library.adelaide.edu.au/theses/09SB/09sbs9715.pdf.
Повний текст джерелаThompson, C. "Thermal and exhumation history of the central Yorke Peninsula, southern Gawler Craton." Thesis, 2013. http://hdl.handle.net/2440/106460.
Повний текст джерелаThe central Yorke Peninsula, South Australia, is a prospective area for iron-oxide-copper-gold mineralisation. However due to minimal exposure there is limited data on the metamorphic, deformation and cooling history on the Central Yorke Peninsula in southern Gawler Craton in southern Australia. Here we use metamorphic zircon and monazite grains from drill holes in the Equis and Ranald prospects to determine the thermal history of the area. U-Pb geochronology suggests that central Yorke Peninsula underwent metamorphism during ca 1540 – 1480 Ma. Pressure – temperature (P-T) modelling suggests that the metamorphic conditions for this thermal event were high temperature/low pressure, amphibolite-granulite facies associated with normal to elevated geothermal gradients. The tectonothermal driver for this event is not clear, it can be suggested that a combination of extension and magmatism may be have contributed to this thermal event. After the thermal event the central Yorke Peninsula underwent a period of extension and exhumation. Exhumation and extension was most likely accommodated by the Pine Point Fault during ca 1500 – 1450 Ma and was likely to be associated with reactivation of major structures, brittle faulting and regional folding in the Gawler Craton. Ca 1600 – 1570 Ma Hiltaba-age mineralisation has possibly been affected by the ca 1540 to 1480 thermal event in ways of remobilisation and concentration and following that was possibly redistributed along the Pine Point Fault during the ca 1500 – 1450 Ma extension and exhumation.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2013
Budd, Anthony. "The Tarcoola Goldfield of the Central Gawler Gold Province, and the Hiltaba Association Granites, Gawler Craton, South Australia." Phd thesis, 2006. http://hdl.handle.net/1885/12890.
Повний текст джерелаKlingberg, L. L. "Regolith-landforms and regolith geochemistry of the ‘Tomahawk’ Au-in-calcrete anomaly: Tunkillia, Gawler Craton, South Australia." Thesis, 2009. http://hdl.handle.net/2440/129278.
Повний текст джерелаThe ‘Tomahawk’ Au-in-calcrete anomaly is a zone of peak Au-in-calcrete content within the Tunkillia prospect of the central Gawler Craton, South Australia. Exploration drilling of this area has failed to intersect significant underlying mineralisation, making this an important setting to investigate controls on linkages between Au-in-calcrete expression and possible mineralisation sources. This study is the first to consider the multi-element geochemical characteristics of calcretes at ‘Tomahawk’ rather than using the Au-only approach of previous geochemical exploration. This investigation also considers the potential for laterally dispersed geochemical signatures across the landscape recorded at the surface of Au and associated elements, and suggests that Au was, and may still be physically mobilised along old and contemporary alluvial drainage depressions. There is a low relief, but locally significant drainage divide to the south of ‘Tomahawk’, so the anomaly area is associated with a point of low, broad confluence of several north flowing palaeodrainage depressions. The interpretation of these palaeolandscape controls further builds on palaeodrainage channel identification from previous studies and supports hypotheses that ‘Tomahawk’ is in an upper catchment setting, relative to the ‘Area 191’ Au-in-calcrete anomaly. Primary Au mineralisation at Tunkillia is associated with pyrite, minor galena and sphalerite within quartz-sulphide veins, and has a geochemical association with Au, Ag, Pb and Zn. Supergene Au enrichment has been recognised within ferruginised saprock overlying mineralised bedrock, and this is largely considered Au-only mineralisation. The calcrete geochemistry here shows some distinction between possible primary and secondary Au occurrences based in the trace element characteristics. The Au-in-calcrete concentrations obtained in this study are up to 194 ppb within CHep and ISps2 regolith-landforms in the north of the study area, corresponding to the lower margins of topography and areas interpreted to be within palaeodrainage systems. Silver concentrations above detection were found in association with many of the elevated Au results, therefore identifying areas of interest and possible alteration halos surrounding primary Au mineralisation. Furthermore, small exposures of weathered in situ quartz veins support a possible source for the ‘Tomahawk’ Au-in-calcrete anomaly to the south, which is immediately upslope of the palaeodrainage system.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2009