A Chemical and Multi-Isotope Study of the Western Cape Olivine Melilitite Province, South Africa: Implications for the Sources of Kimberlites and the Origin of the HIMU Signature in Africa |
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Authors: | JANNEY, P. E. LE ROEX, A. P. CARLSON, R. W. VILJOEN, K. S. |
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Affiliation: | 1DEPARTMENT OF GEOLOGICAL SCIENCES, UNIVERSITY OF CAPE TOWN, RONDEBOSCH 7700, SOUTH AFRICA 2DEPARTMENT OF TERRESTRIAL MAGNETISM, CARNEGIE INSTITUTION OF WASHINGTON, 5241 BROAD BRANCH ROAD, NW, WASHINGTON, DC 20015, USA 3BERNARD PRICE INSTITUTE OF GEOPHYSICAL RESEARCH, UNIVERSITY OF THE WITWATERSRAND, JOHANNESBURG, 2050, SOUTH AFRICA |
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Abstract: | We present major and trace element and SrNdPbHfOsisotopic data for the 7658 Ma Western Cape melilititeprovince, an age-progressive magmatic lineation in which primitiveolivine melilitite intrusives and alkali basalt lavas have beenemplaced on the southwestern margin of South Africa. The magmasrange from alkali basalts with strong HIMU isotopic and traceelement affinities on the continental shelf to melilitites withkimberlite-like incompatible element compositions and EM 1 isotopicaffinities on thick Proterozoic lithosphere (i.e. 87Sr/86Sri= 0·70290·7043, |
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