Low-calcium garnet harzburgites from southern Africa. their relations to craton structure and diamond crystallization

Low-calcium garnet harzburgite xenoliths from the Kaapvaal craton in southern Africa were analyzed. Low-calcium garnets in harzburgite xenoliths are distinct from those that crystallized with diamonds either as inclusions or as grains in diamondiferous kimberlites that disaggregated during eruption.

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Veröffentlicht in:Contributions to mineralogy and petrology 1993-03, Vol.113 (3), p.352-366
Hauptverfasser: BOYD, F. R, PEARSON, D. G, NIXON, P. H, MERTZMAN, S. A
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Sprache:eng
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Zusammenfassung:Low-calcium garnet harzburgite xenoliths from the Kaapvaal craton in southern Africa were analyzed. Low-calcium garnets in harzburgite xenoliths are distinct from those that crystallized with diamonds either as inclusions or as grains in diamondiferous kimberlites that disaggregated during eruption.
ISSN:0010-7999
1432-0967
DOI:10.1007/BF00286927