D/H Ratio Ion Probe Measurements on Magmatic Minerals from Martian Meteorites: Implications for Degassing of the Martian Mantle

Details D/H Ratio Ion Probe Measurements on Magmatic Minerals from Martian Meteorites: Implications for Degassing of the Martian Mantle D/H Ratio Ion Probe Measurements on Magmatic Minerals from Martian Meteorites: Implications for Degassing of the Martian Mantle

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1607d&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1607

Computer Science

2

Scientific paper

Ion probe measurements of D/H ratios in magmatic minerals from 5 Martian
meteorites give low deltaD values, suggesting that the Martian mantle is
not yet completely degassed, and high deltaD values due to their
alteration by Martian surface water.

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