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Статті в журналах з теми "Kanmantoo Group"
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.
Повний текст джерелаJago, 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.
Повний текст джерелаSeccombe, 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.
Повний текст джерелаHaines, 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.
Повний текст джерелаJago, 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.
Повний текст джерелаJago, 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.
Повний текст джерелаTott, 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.
Повний текст джерелаConn, 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.
Повний текст джерелаJago, 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.
Повний текст джерелаTurner, 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.
Повний текст джерелаДисертації з теми "Kanmantoo Group"
Boord, R. A. "Sedimentology of the Cambrian, Upper Kanmantoo Group, Southern Fleurieu Peninsula, South Australia /." Title page, contents and abstract only, 1985. http://web4.library.adelaide.edu.au/theses/09AR/09arb724.pdf.
Повний текст джерелаCannon, Tim P. "Parameters controlling fracturing in the Upper Kanmantoo Group at Coolawang Point, Southern Fleurieu Peninsula /." Title page, contents and abstract only, 1994. http://web4.library.adelaide.edu.au/theses/09SB/09sbc226.pdf.
Повний текст джерелаMadigan, Tania L. A. "The Rathjen gneiss : constraints on the tectonic history of the Kanmantoo Group around Springton, South Australia /." Title page, table of contents and abstract only, 1988. http://web4.library.adelaide.edu.au/theses/09AR/09arm182.pdf.
Повний текст джерелаRajagopalan, Shanti. "Aeromagnetic interpretation of the Kanmantoo Group, South Australia / Shanti Rajagopalan." Thesis, 1989. http://hdl.handle.net/2440/19036.
Повний текст джерелаxi, 128 leaves : ill., maps (some col.), 1 folded ; 30 cm. + 2 microfiche, 5 maps (folded), appendix and errata in pocket inside back cover.
Thesis (Ph.D.)--University of Adelaide, Dept. of Geology and Geophysics, 1989
Rajagopalan, Shanti. "Aeromagnetic interpretation of the Kanmantoo Group, South Australia / Shanti Rajagopalan." 1989. http://hdl.handle.net/2440/19036.
Повний текст джерелаBibliography: leaves 115-128.
xi, 128 leaves : ill., maps (some col.), 1 folded ; 30 cm. + 2 microfiche, 5 maps (folded), appendix and errata in pocket inside back cover.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
Thesis (Ph.D.)--Dept. of Geology and Geophysics, University of Adelaide, 1989
Schiller, Jeffrey Christopher. "Structural geology, metamorphism and origin of the Kanmantoo Copper deposit, South Australia / by Jeffrey Christopher Schiller." 2000. http://hdl.handle.net/2440/19902.
Повний текст джерелаIncludes copies of articles co-authored by the author during the preparation of this thesis as appendix 7.
14 maps (some folded, some col.); inserted in back pocket.
Includes bibliographical references (leaves 242-264).
System requirements for accompanying CD-ROM: Macintosh of IBM compatible computer. Other requirements: Adobe Acrobat Reader.
[15], 264 leaves : ill. (some col.), maps ; 30 cm. + 1 computer optical disk (4 3/4 in.)
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
On the basis of the present study it is concluded that there is no firm evidence that the bulk of the mineralisation is pre-metamorphic, although the possibility has not been excluded.
Thesis (Ph.D.)--Adelaide University, Dept. of Geology and Geophysics, 2001
Schiller, Jeffrey Christopher. "Structural geology, metamorphism and origin of the Kanmantoo Copper deposit, South Australia." Thesis, 2000. http://hdl.handle.net/2440/19902.
Повний текст джерелаIncludes copies of articles co-authored by the author during the preparation of this thesis as appendix 7.
14 maps (some folded, some col.); inserted in back pocket.
Includes bibliographical references (leaves 242-264).
System requirements for accompanying CD-ROM: Macintosh of IBM compatible computer. Other requirements: Adobe Acrobat Reader.
[15], 264 leaves : ill. (some col.), maps ; 30 cm. + 1 computer optical disk (4 3/4 in.)
On the basis of the present study it is concluded that there is no firm evidence that the bulk of the mineralisation is pre-metamorphic, although the possibility has not been excluded.
Thesis (Ph.D.) -- University of Adelaide, Dept. of Geology and Geophysics, 2001
De, Pretis D. G. "Application of lithogeochemistry to identify stratigraphic units and provenance of the Kanmantoo Group, Kangaroo Island." Thesis, 2008. http://hdl.handle.net/2440/121115.
Повний текст джерелаGeochemical data, including Nd isotope ratios, were used to help establish stratigraphic correlations between Kanmantoo Group sedimentary rocks on the mainland and Kangaroo Island, as well as constrain their provenance. Whole-rock geochemistry of the Kangaroo Island and mainland Kanmantoo Group varied, with little consistency, suggesting a mixed sediment source. The Talisker Formation however has a distinctly higher abundance of mafic detritus compared to other Kanmantoo Group formations. Initial Nd data from the Kangaroo Island Kanmantoo Group is between -12 to -15, compared to those from the mainland which range between -9 and -12 (Turner et al. 1993). The Nd data are similar to basement of the Gawler Craton and east Antarctica (Prydz Bay), which are two possible source terrains for the sediments. Palaeocurrent data on Kangaroo Island indicate a southern provenance. The Nd values of Prydz Bay charnockites and felsic gneisses at around 500 Ma are similar to that of the Kangaroo Island Kanmantoo Group. Results from the outcomes of this study suggest that the Kanmantoo Group was derived from a mixture of sources, including the Gawler Craton, west Antarctica (Ross Orogeny) and Adelaidean rocks. However, there appears to be a dominance of sediment from the east-Gondwana Orogenic belt in east Antarctica.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2008
Randabel, J. P. J. "The geology of the Snug Cove area, north west coast Kangaroo Island, South Australia." Thesis, 1992. http://hdl.handle.net/2440/87108.
Повний текст джерелаOn the north west coast of Kangaroo Island in the vicinity of Snug Cove a major shear - the Snug Cove Shear Zone (SCSZ) has been recognised. The Snug Cove Shear Zone trends east-west in the area but is believed to strike inland to the east. The lithologies in the area were highly foliated and recrystallised in the shear zone but are gently folded outside of it. The lithological descriptions of Daily & Milnes (1971, 1973) were used to determine the stratigraphic position of the Snug Cove rocks; they are most likely to be within the Tapanappa Formation. Flattening strains in the area were low and the strain ellipsoid was oblate to spherical - a result of high recrystallisation. Kinematic indicators indicate a top to the north sense of shear throughout the shear zone. Strain variations in the shear zone are illustrated by the presence of high strain mylonitic zones in between lenticular relatively less deformed zones and the anastomosing nature of the mylonitic foliation. The relationship between the SCSZ and the nearby West Bay Syncline is due to the reactivation of a preexisting fault such that the SCSZ is located on the normal limb of the fold and not on the overturned limb as expected. The localisation of stress to create a ductile to semi-ductile shear zone is attributed to the buttressing effect of the Gawler Craton. Regionally, more than one deformation can be proposed on the basis of foliation relationships in porphyroblast schist. D1 was folding and cleavage development; D2 was crenulation and metamorphism; D3 was shear zone development.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 1992
Pluckhahn, D. "The Palmer Granite: geochronology, geochemistry and genesis." Thesis, 1993. http://hdl.handle.net/2440/87543.
Повний текст джерелаVarious igneous bodies have intruded the Palmer area throughout the Delamerian Orogeny. The earliest, the Rathjen Gneiss, intruded either before or during D1 which gave it the prominent foliation. D1 was also responsible for crenulations in migmatite veins throughout the area. These crenelated migmatite veins are in areas folded by D2 mesoscale folds. Some pegmatite veins are also folded by D2 folds. The Palmer Granite intruded during D2 as is seen by shearing in a semi-crystalline state and a tectonic foliation that has been folded. The ballooning of the granite during emplacement deforms the surrounding sediments and the pre-granite folds hence their axes lie parallel to the contact of the granite. The effect of the granite intruding during the deformation has lead to the axis of the D2 folds forming after the granite to have a degree of randomness about their axis. Migmatite grade was reached again after the intrusion of the granite causing melt veins to develop to disrupt the foliation. D3 formed a regional syncline of the area combined with some small scale folding within the granite, however a foliation did not form. The emplacement of the granite and some other igneous bodies throughout the area has been controlled by using the bedding plane of the Kanmantoo. The geochemical trends throughout the Palmer Granite is formed by two different groups fractionally crystallising zircon, amphibole and biotite. This results in a decrease of normally incompatible elements. The two groups form by one group from a homogeneous source and the other a heterogeneous source. The xenoliths crystallised from a mafic magma. The amphibolites form two groups according to their differentiation and genetic relationship. They both form by fractional crystallisation however U and Pb are decreasing cannot be explained by this. Another possible mechanism is liquid un-mixing. To tie all of the groups together a model of a mafic pluton that crystallises the xenoliths as a chilled margin. The mafic magma evolves some of the Palmer Granite whilst turbulently convecting hence homogenising the magma. A magma recharge forms the more evolved mafic and this forms more Palmer Granite which convects in a laminar fashion forming heterogeneities. Part of the mafics evolve enough to be caught up in the Palmer Granite and as it does not crystallise zircons all the fractional crystallisation of the Palmer Granite must have occurred in the mafic plution.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 1993
Тези доповідей конференцій з теми "Kanmantoo Group"
Conn, C. Dakota, Paul G. Spry, and Alan E. Koenig. "THE GENETIC RELATIONSHIP BETWEEN THE NAIRNE PYRITE MEMBER AND METAMORPHOSED SEDIMENT-HOSTED CU-AU AND PB-ZN-AG DEPOSITS, KANMANTOO GROUP, SOUTH AUSTRALIA." In 52nd Annual North-Central GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018nc-311896.
Повний текст джерелаTott, Katherine A., Paul G. Spry, Meaghan V. MacPherson, Alan E. Koenig, Ross A. Both, and Joseph Ogierman. "TRACE ELEMENT CHEMISTRY OF SILICATES AND OXIDES AS VECTORS TO METAMORPHOSED SEDIMENT-HOSTED PB-ZN-AG AND CU-AU DEPOSITS IN THE CAMBRIAN KANMANTOO GROUP, SOUTH AUSTRALIA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-278369.
Повний текст джерелаЗвіти організацій з теми "Kanmantoo Group"
Spry, P. G., M. V. Pollock, K. A. Tott, A. E. Koenig, R A Both, and J. A. Ogierman. Trace element chemistry of indicator silicates and oxides as vectors to metamorphosed sediment-hosted Pb-Zn-Ag and Cu-Au deposits in the Cambrian Kanmantoo Group, South Australia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2017. http://dx.doi.org/10.4095/306311.
Повний текст джерела