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Oxide, sulphide and carbonate minerals in a mantle polymict breccia: Metasomatism by proto-kimberlite magmas, and relationship to the kimberlite megacrystic suite

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Giuliani, Andrea
Kendrick, Mark
Kamenetsky, Vadim S.
Phillips, David
Wyatt, B. A.
Maas, Roland

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Elsevier

Abstract

Polymict breccias entrained by kimberlites are mantle xenoliths comprising coarse-grained mantle minerals (porphyroclasts) and rock clasts, cemented together by ilmenite, rutile, phlogopite, olivine and minor sulphides. These unusual xenoliths are general

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Chemical Geology

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Restricted until

2037-12-31