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Water on Mars: Clues from Deuterium/Hydrogen and Water Contents of Hydrous Phases in SNC Meteorites
Laurie Leshin Watson, Ian D. Hutcheon, Samuel Epstein and Edward M. Stolper
New Series, Vol. 265, No. 5168 (Jul. 1, 1994), pp. 86-90
Published by: American Association for the Advancement of Science
Stable URL: http://www.jstor.org/stable/2884366
Page Count: 5
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Ion microprobe studies of hydrous amphibole, biotite, and apatite in shergottite-nakhlite-chassignite (SNC) meteorites, probable igneous rocks from Mars, indicate high deuterium/hydrogen (D/H) ratios relative to terrestrial values. The amphiboles contain roughly one-tenth as much water as expected, suggesting that SNC magmas were less hydrous than previously proposed. The high but variable D/H values of these minerals are best explained by postcrystallization D enrichment of initially D-poor phases by martian crustal fluids with near atmospheric D/H (about five times the terrestrial value). These igneous phases do not directly reflect the D/H ratios of martian "magmatic" water but provide evidence for a D-enriched martian crustal water reservoir.
Science © 1994 American Association for the Advancement of Science