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Journal articles on the topic 'Kanmantoo'

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Author: Grafiati

Published: 10 December 2022

Last updated: 28 January 2023

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1

Haines, P. W., J. B. Jago, and J. C. Gum. "Turbidite deposition in the Cambrian Kanmantoo Group, South Australia." Australian Journal of Earth Sciences 48, no. 3 (June 2001): 465–78. http://dx.doi.org/10.1046/j.1440-0952.2001.00872.x.

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2

Parker, A. J. "Tectonic development and metallogeny of the Kanmantoo Trough in South Australia." Ore Geology Reviews 1, no. 2-4 (November 1986): 203–12. http://dx.doi.org/10.1016/0169-1368(86)90009-0.

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3

Jago, J. B., and C. G. Gatehouse. "The Type Section of the Cambrian Backstairs Passage Formation, Kanmantoo Group, South Australia." Transactions of the Royal Society of South Australia 133, no. 1 (January 2009): 150–63. http://dx.doi.org/10.1080/03721426.2009.10887114.

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4

Seccombe, P. K., P. G. Spry, R. A. Both, M. T. Jones, and J. C. Schiller. "Base metal mineralization in the Kanmantoo Group, South Australia; a regional sulfur isotope study." Economic Geology 80, no. 7 (November 1, 1985): 1824–41. http://dx.doi.org/10.2113/gsecongeo.80.7.1824.

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5

Pollock, Meaghan V., Paul G. Spry, Katherine A. Tott, Alan Koenig, Ross A. Both, and Joseph Ogierman. "The origin of the sediment-hosted Kanmantoo Cu-Au deposit, South Australia: Mineralogical considerations." Ore Geology Reviews 95 (April 2018): 94–117. http://dx.doi.org/10.1016/j.oregeorev.2018.02.017.

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6

Haines, P. W., S. P. Turner, J. D. Foden, and J. B. Jago. "Isotopic and geochemical characterisation of the Cambrian Kanmantoo Group, South Australia: implications for stratigraphy and provenance." Australian Journal of Earth Sciences 56, no. 8 (December 2009): 1095–110. http://dx.doi.org/10.1080/08120090903246212.

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7

Jago, J. B., I. A. Dyson, and C. G. Gatehouse. "The nature of the sequence boundary between the Normanville and Kanmantoo Groups on Fleurieu Peninsula, South Australia." Australian Journal of Earth Sciences 41, no. 5 (October 1994): 445–53. http://dx.doi.org/10.1080/08120099408728154.

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8

Jago, J. B., and C. G. Gatehouse. "Early Cambrian trace fossils from the Kanmantoo Group at Red Creek, South Australia, and their stratigraphic significance." Australian Journal of Earth Sciences 54, no. 4 (June 2007): 531–40. http://dx.doi.org/10.1080/08120090601078370.

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9

Smith, Robert J. "Geophysics in Australian mineral exploration." GEOPHYSICS 50, no. 12 (December 1985): 2637–65. http://dx.doi.org/10.1190/1.1441888.

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I review a variety of recent case histories illustrating the application of geophysics in mineral exploration in Australia. Geophysics is now an integral part of most programs. Examples are given of contributions by geophysics to all stages of mineral exploration, from regional area selection through to mine planning and development. Specific case histories summarized are as follows: (a) Olympic Dam copper‐uranium‐gold deposit, discovered using a conceptual genetic model and regional geophysical data; (b) Ellendale diamondiferous kimberlites, illustrating the use of low level, detailed airborne magnetics; (c) Ranger uranium orebodies, discovered by detailed airborne radiometric surveys; (d) geologic mapping near Mary Kathleen with color displays of airborne radiometric data; (e) mapping of lignite in basement depressions of the Bremer Basin, near Esperance, with INPUT; (f) White Leads, a lead‐zinc sulfide deposit discovered with induced polarization (IP) and TEM, near Broken Hill; (g) Hellyer, a lead‐zinc‐silver‐gold deposit discovered with UTEM; (h) application of geophysical logging near Kanmantoo; (i) Cowla Peak, a subbituminous steaming coal deposit mapped with ground TEM; and (j) Cook Colliery, where high‐resolution seismic reflection methods have successfully increased the workable reserves.

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10

Oliver, N. H. S., G. M. Dipple, I. Cartwright, and J. Schiller. "Fluid flow and metasomatism in the genesis of the amphibolites-facies, pelite-hosted Kanmantoo copper deposit, South Australia." American Journal of Science 298, no. 3 (March 1, 1998): 181–218. http://dx.doi.org/10.2475/ajs.298.3.181.

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11

FLÖTTMANN, T., P. HAINES, J. JAGO, P. JAMES, A. BELPERIO, and J. GUM. "Formation and reactivation of the Cambrian Kanmantoo Trough, SE Australia: implications for early Palaeozoic tectonics at eastern Gondwana’s plate margin." Journal of the Geological Society 155, no. 3 (May 1998): 525–39. http://dx.doi.org/10.1144/gsjgs.155.3.0525.

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12

Jago, J. B., J. C. Gum, A. C. Burtt, and P. W. Haines. "Stratigraphy of the Kanmantoo Group: A critical element of the Adelaide Fold Belt and the Palaeo‐Pacific plate margin, Eastern Gondwana." Australian Journal of Earth Sciences 50, no. 3 (June 2003): 343–63. http://dx.doi.org/10.1046/j.1440-0952.2003.00997.x.

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13

Tedesco, Adam. "Late-stage orogenic model for Cu-Au mineralisation at Kanmantoo mine: New insights from titanium in quartz geothermometry, fluid inclusions and geochemical modelling." Journal of Geochemical Exploration 101, no. 1 (April 2009): 103. http://dx.doi.org/10.1016/j.gexplo.2008.11.043.

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14

Tott, Katherine A., Paul G. Spry, Meaghan V. Pollock, Alan Koenig, Ross A. Both, and Joseph Ogierman. "Ferromagnesian silicates and oxides as vectors to metamorphosed sediment-hosted Pb-Zn-Ag-(Cu-Au) deposits in the Cambrian Kanmantoo Group, South Australia." Journal of Geochemical Exploration 200 (May 2019): 112–38. http://dx.doi.org/10.1016/j.gexplo.2019.01.015.

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15

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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16

Focke, D., A. Schmidt Mumm, A. Tedesco, T. Seifert, and R. Bradey. "Pressure, temperature and fluid composition variation of the mineralising system at the Kanmantoo Cu-Au deposit: Combining fluid inclusion analysis with Ti in quartz thermometry." Journal of Geochemical Exploration 101, no. 1 (April 2009): 35. http://dx.doi.org/10.1016/j.gexplo.2008.11.026.

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17

de Caritat, Patrice, Anthony Dosseto, and Florian Dux. "A strontium isoscape of inland southeastern Australia." Earth System Science Data 14, no. 9 (September 22, 2022): 4271–86. http://dx.doi.org/10.5194/essd-14-4271-2022.

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Abstract. The values and distribution patterns of the strontium (Sr) isotope ratio 87Sr/86Sr in Earth surface materials are of use in the geological, environmental, and social sciences. Ultimately, the 87Sr/86Sr ratios of soils and everything that lives in and on them are inherited from the rocks that are the parent materials of the soil's components. In Australia, there are few large-scale surveys of 87Sr/86Sr available, and here we report on a new, low-density dataset using 112 catchment outlet (floodplain) sediment samples covering 529 000 km2 of inland southeastern Australia (South Australia, New South Wales, Victoria). The coarse (<2 mm) fraction of bottom sediment samples (depth ∼ 0.6–0.8 m) from the National Geochemical Survey of Australia were milled and fully digested before Sr separation by chromatography and 87Sr/86Sr determination by multicollector-inductively coupled plasma mass spectrometry. The results show a wide range of 87Sr/86Sr values from a minimum of 0.7089 to a maximum of 0.7511 (range 0.0422). The median 87Sr/86Sr (± median absolute deviation) is 0.7199 (± 0.0071), and the mean (± standard deviation) is 0.7220 (± 0.0106). The spatial patterns of the Sr isoscape observed are described and attributed to various geological sources and processes. Of note are the elevated (radiogenic) values (≥∼ 0.7270; top quartile) contributed by (1) the Palaeozoic sedimentary country rock and (mostly felsic) igneous intrusions of the Lachlan geological region to the east of the study area; (2) the Palaeoproterozoic metamorphic rocks of the central Broken Hill region; both these sources contribute radiogenic material mainly by fluvial processes; and (3) the Proterozoic to Palaeozoic rocks of the Kanmantoo, Adelaide, Gawler, and Painter geological regions to the west of the area; these sources contribute radiogenic material mainly by aeolian processes. Regions of low 87Sr/86Sr (≤∼ 0.7130; bottom quartile) belong mainly to (1) a few central Murray Basin catchments; (2) some Darling Basin catchments in the northeast; and (3) a few Eromanga geological region-influenced catchments in the northwest of the study area; these sources contribute unradiogenic material mainly by fluvial processes. The new spatial Sr isotope dataset for the DCD (Darling–Curnamona–Delamerian) region is publicly available (de Caritat et al., 2022; https://dx.doi.org/10.26186/146397).

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18

Teasdale, J. P., L. L. Pryer, P. G. Stuart-Smith, K. K. Romine, M. A. Etheridge, T. S. Loutit, and D. M. Kyan. "STRUCTURAL FRAMEWORK AND BASIN EVOLUTION OF AUSTRALIA’S SOUTHERN MARGIN." APPEA Journal 43, no. 1 (2003): 13. http://dx.doi.org/10.1071/aj02001.

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The structural evolution of all of the Southern Margin Basins can be explained by episodic reactivation of basement structures in respect to a specific sequence of tectonic events. Three geological provinces dominate the basement geology of the Southern Margin basins. The Eyre, Ceduna, Duntroon and Polda Basins overlie basement of the Archean to Proterozoic Gawler-Antarctic Craton. The Otway and Sorell Basins overlie basement of the Neoproterozoic-early Palaeozoic Adelaide- Kanmantoo Fold Belt. The Bass and Gippsland Basins overlie basement of the Palaeozoic Lachlan Fold Belt. The contrasting basement terranes within the three basement provinces and the structures within and between them significantly influenced the evolution and architecture of the Southern Margin basins.The present-day geometry was established during three Mesozoic extensional basin phases:Late Jurassic–Early Cretaceous NW–SE transtension forming deep rift basins to the west and linked pullapart basins and oblique graben east of the Southwest Ceduna Accommodation Zone; Early–Mid Cretaceous NE–SW extension; and Late Cretaceous NNE–SSW extension leading to continental breakup. At least three, potentially trap forming, inversion events have variably influenced the Southern Margin basins; Mid Cretaceous, Eocene, and Miocene-Recent. Volcanism occurred along the margin during the Late Cretaceous and sporadically through the Tertiary.First-order structural control on Mesozoic rifting and breakup were east–west trending basement structures of the southern Australian fracture zone. Second-order controls include:Proterozoic basement shear zones and/or terrane boundaries in the western Gawler Craton, which controlled basin evolution in the Eyre and Ceduna Subbasins; Neoproterozoic structures, which significantly influenced basin evolution in the Ceduna sub-basin; Cambro-Ordovician basement shear zones and/or terrane boundaries, which were a primary control on basin evolution in the Otway and Sorell Basins; and Palaeozoic structures in the Lachlan Fold Belt, which controlled basin evolution in the Bass and Gippsland Basins.A SEEBASE™ (Structurally Enhanced view of Economic Basement) model for the Southern Margin basins has been constructed to show basement topography. When used in combination with a rigorous interpretation of the structural evolution of the margin, it provides a foundation for basin phase and source rock distribution, hydrocarbon fluid focal points and trap type/distribution.

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19

Turner, Simon, Trevor Ireland, John Foden, Elena Belousova, Gerhard Wörner, and Jelte Keeman. "A comparison of granite genesis in the Adelaide Fold Belt and Glenelg River Complex using U-Pb, Hf and O isotopes in zircon." Journal of Petrology, October 11, 2022. http://dx.doi.org/10.1093/petrology/egac102.

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Abstract We present new U-Pb ages and Hf and O isotope data for zircon from I-, S- and A-type granites from both the western and eastern edges of the Delamerian Orogen in southeastern Australia. The I-type Tanunda Creek Gneiss contains zircon populations of 507 ± 4 Ma and 492 ± 6 Ma inferred to reflect igneous and metamorphic ages, respectively. The I-type Palmer Granite yielded an age of 509 ± 3 Ma and the Port Elliot S-type Granite has a magmatic age of 508 ± 7 Ma. Inherited zircon in these granites range from 1092 to 3343 Ma, probably derived from assimilation of Adelaide Group sediments. The Murray Bridge A-type Granite is 490 ± 2 Ma in age and lacks inherited zircon. In the Glenelg River Complex, a S-type migmatite from near Harrow contains a complex zircon population. It is most likely ~ 500 Ma in age and has inherited zircon of 550-700, 1000-1100 and 2437 Ma, hence matching those from the Kanmantoo Group. From this and detrital zircons ages we infer that only the Kanmantoo Group extends across the Murray Basin into the Glenelg River Complex. The Wando Tonalite and Loftus Creek I-type granites yielded ages of 501 ± 2 Ma and 486 ± 3 Ma, respectively. Zircon from the Dergholm Granite has suffered Pb loss and the best age estimate for this granite is 488 ± 5 Ma. Combining all the granite data together, εHft and δ18O in the magmatic zircon range from 5.6 to -10.3 and from 5.8 to 8.1, respectively, and are well correlated. The zircon indicate the same temporal and compositional evolution of granitic petrogenesis across ~ 300 km of strike, reaffirming the notion that these terranes form part of the same orogen. Westward-directed subduction caused orogenic thickening, heating and increasing amounts of crustal contribution. This was followed by convective thinning of the thickened mantle lithosphere and a return to more primitive magmas lacking significant crustal contributions. It contrasts significantly with inferred granite petrogenesis and tectonic style in the younger Lachlan and New England Fold Belts further east that were not built upon extended cratonic lithosphere.

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20

"Formation and reactivation of the Cambrian Kanmantoo Trough, SE Australia: implications for early Palaeozoic tectonics at eastern Gondwana's plate margin." Journal of African Earth Sciences 27, no. 3-4 (October 1998): XIV. http://dx.doi.org/10.1016/s0899-5362(98)90646-7.

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