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...
| Hlavní autoři: | , , , |
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| Médium: | Journal article |
| Vydáno: |
European Association of Geochemistry
2015
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