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...

Ful tanımlama

Detaylı Bibliyografya
Asıl Yazarlar: Kiseeva, E, Wood, B, Ghosh, S, Stachel, T
Materyal Türü: Journal article
Baskı/Yayın Bilgisi: European Association of Geochemistry 2015

Benzer Materyaller