Fluorine, Chlorine and Water Fugacities in Planetary Basalts Recorded by Phosphate Equilibria

Details Fluorine, Chlorine and Water Fugacities in Planetary Basalts Recorded by Phosphate Equilibria Fluorine, Chlorine and Water Fugacities in Planetary Basalts Recorded by Phosphate Equilibria

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.2037p&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.2037

Computer Science

Scientific paper

We use apatite-merrillite equilibria to compare the relative values of
halogen (F, Cl) and water fugacities in martian, lunar, eucritic and
terrestrial basalts and conclude that the martian mantle is depleted in
Cl and water compared to the terrestrial mantle.

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