Computer Science
Scientific paper
Mar 1992
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992sci...255.1409k&link_type=abstract
Science (ISSN 0036-8075), vol. 255, March 13, 1992, p. 1409-1411.
Computer Science
55
Mars Atmosphere, Mars Environment, Meteoritic Composition, Moisture Content, Mars Surface, Oxygen Isotopes, Planetary Crusts, Planetary Geology, Water Vapor
Scientific paper
The Shergotty-Nakhla-Chassigny (SNC) meteorites, purportedly of Martian origin, contain 0.04 to 0.4 percent water by weight. Oxygen isotopic analysis can be used to determine whether this water is extraterrestrial or terrestrial. Such analysis reveals that a portion of the water is extraterrestrial and furthermore was not in oxygen isotopic equilibrium with the host rock. Lack of equilibrium between water and host rock implies that the lithosphere and hydrosphere of the SNC parent body formed two distinct oxygen isotopic reservoirs. If Mars was the parent body, the maintenance of two distinct reservoirs may result from the absence of plate tectonics on the planet.
Clayton Robert N.
Gibson Everett K. Jr.
Karlsson Haraldur R.
Mayeda Toshiko K.
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