Trace elements in olivine and the petrogenesis of the intermediate, olivine‐phyric shergottite NWA 10170

Olivine‐phyric shergottites represent primitive basaltic to picritic rocks, spanning a large range of Mg# and olivine abundances. As primitive olivine‐bearing magmas are commonly representative of their mantle source on Earth, understanding the petrology and evolution of olivine‐phyric shergottites...

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Veröffentlicht in:	Meteoritics & planetary science 2017-02, Vol.52 (2), p.391-409
Hauptverfasser:	Howarth, Geoffrey H., Udry, Arya
Format:	Artikel
Sprache:	eng
Schlagworte:	Chambers Magma Mantle Melts Nickel Olivine Shergottites Trace elements
Online-Zugang:	Volltext
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