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...
Główni autorzy: | Kiseeva, E, Wood, B, Ghosh, S, Stachel, T |
---|---|
Format: | Journal article |
Wydane: |
European Association of Geochemistry
2015
|
Podobne zapisy
-
The roles of pyroxenite and peridotite in the mantle sources of oceanic basalts
od: Matzen, A, i wsp.
Wydane: (2017) -
Geochemistry of forty‐one eclogitic and pyroxenitic mantle xenoliths from the Central Slave Craton, Canada (Ekati Diamond Mine)
od: D. E. Jacob, i wsp.
Wydane: (2024-10-01) -
The roles of 1herzolite and garnet pyroxenite in the constitution of the upper mantle,
od: Reid, John Barlow
Wydane: (2010) -
Petrology and geochemistry of pyroxenites in the Lanzo ultramafic massif, Northwestern Italy
od: Pesce, Kathryn A
Wydane: (2012) -
Melts of garnet lherzolite: experiments, models and comparison to melts of pyroxenite and carbonated lherzolite
od: Grove, Timothy L., i wsp.
Wydane: (2016)