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Marsh, J.S. (2003) The geochemical structure of the Insizwa lobe of the Mount Ayliff complex with implications for the emplacement and evolution of the complex and its Ni-sulphide potential. South African Journal of Geology, 106 (4) 409-428 doi:10.2113/106.4.409

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Reference TypeJournal (article/letter/editorial)
TitleThe geochemical structure of the Insizwa lobe of the Mount Ayliff complex with implications for the emplacement and evolution of the complex and its Ni-sulphide potential
JournalSouth African Journal of Geology
AuthorsMarsh, J.S.Author
Year2003 (December 1)Volume106
Issue4
PublisherGeological Society of South Africa
DOIdoi:10.2113/106.4.409Search in ResearchGate
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Mindat Ref. ID505174Long-form Identifiermindat:1:5:505174:2
GUID0
Full ReferenceMarsh, J.S. (2003) The geochemical structure of the Insizwa lobe of the Mount Ayliff complex with implications for the emplacement and evolution of the complex and its Ni-sulphide potential. South African Journal of Geology, 106 (4) 409-428 doi:10.2113/106.4.409
Plain TextMarsh, J.S. (2003) The geochemical structure of the Insizwa lobe of the Mount Ayliff complex with implications for the emplacement and evolution of the complex and its Ni-sulphide potential. South African Journal of Geology, 106 (4) 409-428 doi:10.2113/106.4.409
In(2003, December) South African Journal of Geology Vol. 106 (4) Geological Society of South Africa

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LocalityCitation Details
Insizwa, Umzimvubu Local Municipality, Alfred Nzo District Municipality, Eastern Cape, South Africa
Mount Ayliff Complex, South Africa

See Also

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Maier, W. D., Marsh, J. S., Barnes, S.-J., Dodd, D. C. (2002) The Distribution of Platinum Group Elements in the Insizwa Lobe, Mount Ayliff Complex, South Africa: Implications for Ni-Cu-PGE Sulfide Exploration in the Karoo Igneous Province. Economic Geology, 97 (6) 1293-1306 doi:10.2113/gsecongeo.97.6.1293
Cawthorn, R. G., Kruger, F. J. (2004) PETROLOGY AND Ni Cu PGE POTENTIAL OF THE INSIZWA LOBE, MOUNT AYLIFF INTRUSION, SOUTH AFRICA. The Canadian Mineralogist, 42 (2) 303-324 doi:10.2113/gscanmin.42.2.303
Marsh, J.S. (2003) Implications of a new 40Ar/ 39Ar age for a basalt flow interbedded with the Etjo Formation, Northeast Namibia. South African Journal of Geology, 106 (4) 281-286 doi:10.2113/106.4.281
Sander, B.K., Cawthorn, R.G. (1996) 2.5-D gravity model of the Niî—¸Cuî—¸PGM mineralized Mount Ayliff Intrusion (Insizwa Complex), South Africa. Journal of Applied Geophysics, 35 (1) 27-43 doi:10.1016/0926-9851(95)00027-5
Maier, W. D. (2003) The potential for magmatic Ni sulfide ores in South African komatiites: a review. South African Journal of Geology, 106 (1) 35-40 doi:10.2113/1060035
Maier, W.D., Barnes, S.-J., Ashwal, L.D., Li, C. (2001) A reconnaissance study on the magmatic Cu-Ni-PGE sulphide potential of the Tete Complex, Mozambique. South African Journal of Geology, 104 (4) 355-363 doi:10.2113/gssajg.104.4.355
Lightfoot, P.C. and Naldrett, A.J., (1983) The geology of the Tabankulu section of the Insizwa Complex, Transkei, southern Africa, with reference to the nickel sulphide potential. Transactions of the Geological Society of South Africa, 86(3), 169-188.
Basson, I.J. (2003) Structural overview of selected Group II kimberlite dyke arrays in South Africa: implications for kimberlite emplacement mechanisms. South African Journal of Geology, 106 (4) 375-394 doi:10.2113/106.4.375
Hornsey, R.A. (2025) The Merensky Reef of the Bushveld Complex, South Africa: Mineral systems analysis of its emplacement and timing of the PGE-Ni-Cu mineralisation. South African Journal of Geology, 128 (3). doi:10.25131/sajg.128.0013
Bailie, R.H., Robb, L.J. (2004) Polymetallic mineralization in the granites of the Bushveld Complex - examples from the central southeastern lobe. South African Journal of Geology, 107 (4) 633-652 doi:10.2113/gssajg.107.4.633
Barton, J.M. (2003) The geology of the area surrounding the Venetia kimberlite pipes, Limpopo Belt, South Africa: A complex interplay of nappe tectonics and granitoid magmatism. South African Journal of Geology, 106 (2) 109-128 doi:10.2113/106.2-3.109
 
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