Ultramafic rocks in the centre of the Vredefort structure (South Africa): geochemical affinity to Bushveld rocks
The geochemistry and mineral chemistry of ultramafic rocks in the centre of the Vredefort structure have been reinterpreted. A detailed examination of previously published major element, trace and REE analyses as well as mineral analyses strongly suggests a magmatic origin in contrast to previously...
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Published in | Chemical geology Vol. 143; no. 1; pp. 43 - 64 |
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Main Authors | , |
Format | Journal Article |
Language | English |
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Elsevier B.V
17.11.1997
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Abstract | The geochemistry and mineral chemistry of ultramafic rocks in the centre of the Vredefort structure have been reinterpreted. A detailed examination of previously published major element, trace and REE analyses as well as mineral analyses strongly suggests a magmatic origin in contrast to previously postulated tectonic emplacement of mantle material. A strong geochemical affinity to ultramafic rocks from the Bushveld Complex is evident. The magmatic nature of the ultramafic rocks in the centre of the Vredefort structure has implications for the discussion of the metamorphic history of the Vredefprt structure which shows evidence of unusually high, and as yet not satisfactorily explained, geothermal gradients during peak metamorphism. |
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AbstractList | The geochemistry and mineral chemistry of ultramafic rocks in the centre of the Vredefort structure have been reinterpreted. A detailed examination of previously published major element, trace and REE analyses as well as mineral analyses strongly suggests a magmatic origin in contrast to previously postulated tectonic emplacement of mantle material. A strong geochemical affinity to ultramafic rocks from the Bushveld Complex is evident. The magmatic nature of the ultramafic rocks in the centre of the Vredefort structure has implications for the discussion of the metamorphic history of the Vredefprt structure which shows evidence of unusually high, and as yet not satisfactorily explained, geothermal gradients during peak metamorphism. |
Author | Merkle, R.K.W. Wallmach, T. |
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Cites_doi | 10.1029/JB093iB03p02191 10.1180/minmag.1977.041.318.12 10.1016/0009-2541(90)90282-C 10.1130/0091-7613(1995)023<0277:MANTCO>2.3.CO;2 10.1016/0040-1951(90)90091-L 10.1002/gj.3350300311 10.1029/JB086iB11p10639 10.1016/0009-2541(90)90072-F 10.2113/gsecongeo.77.6.1296 10.1016/0016-7037(76)90199-X 10.1016/S0301-9268(96)00043-5 10.1086/627516 10.1016/0040-1951(90)90089-Q 10.1111/j.1525-1314.1987.tb00387.x 10.2113/gsecongeo.80.4.849 10.1016/0040-1951(90)90090-U 10.1016/0012-821X(82)90122-4 10.1016/0899-5362(95)00112-3 10.1016/0016-7037(84)90192-3 10.2475/ajs.261.7.597 10.1016/0899-5362(94)90068-X 10.1007/BF00373080 10.1016/0040-1951(90)90088-P 10.2113/gsecongeo.78.7.1287 10.5408/0022-1368-41.2.106 10.1111/j.1945-5100.1995.tb01132.x 10.2113/gsecongeo.80.4.813 10.1029/JB081i023p04247 10.1007/BF00375446 10.1016/0040-1951(90)90098-S 10.1016/0169-1368(94)90017-5 |
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Keywords | ultramafic Vredefort South Africa geochemistry Bushveld Complex origin |
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Title | Ultramafic rocks in the centre of the Vredefort structure (South Africa): geochemical affinity to Bushveld rocks |
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