Xenoliths evidence for a refractory oceanic mantle percolated by basaltic melts beneath the Kerguelen archipelago

Alkali basalts from the Kerguelen islands have entrained many mantle peridotites (harzburgites and dunites) in addition to various other ultramafic and mafic xenoliths. The harzburgites and the dunites were equilibrated in the spinel peridotite stability field (T = 850-1150°C). They attest to the ex...

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Bibliographic Details
Main Authors: Grégoire, Michel, Lorand, Jean Pierre, Cottin, Jean Yves, Giret, André, Mattielli, Nadine, Weis, Dominique
Format: Article in Journal/Newspaper
Language:English
Published: 1997
Subjects:
Online Access:https://researchers.mq.edu.au/en/publications/15a41d24-bd82-4c0a-81e3-0db1a50b2288
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