The pyroxenite-diamond connection

The pyroxenite-diamond connection

Pieces of the Earth’s mantle occurring either as tectonic fragments or xenoliths in volcanic rocks are dominantly peridotites, assemblages of olivine, ortho- and clinopyroxene with minor garnet and/or spinel. They frequently contain pyroxene-rich inclusions which have compositions intermediate betwe...

Bibliografiset tiedot
Päätekijät:	Kiseeva, E, Wood, B, Ghosh, S, Stachel, T
Aineistotyyppi:	Journal article
Julkaistu:	European Association of Geochemistry 2015

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