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 |
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Hauptverfasser: | , , , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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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. |
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ISSN: | 0010-7999 1432-0967 |
DOI: | 10.1007/BF00286927 |