Depletion of Vanadium in Planetary Mantles: Controlled by Metal, Oxide, or Silicate?

Details Depletion of Vanadium in Planetary Mantles: Controlled by Metal, Oxide, or Silicate? Depletion of Vanadium in Planetary Mantles: Controlled by Metal, Oxide, or Silicate?

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.2259r&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.2259

Computer Science

Scientific paper

Vanadium can be compatible in both FeNi metal and mantle phases such as
spinel, magnesiowustite and garnet. In this paper consideration of
depletions due to metal, oxide and silicate are critically evaluated and
applied to Earth, Moon, Mars and Vesta.

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