Martian atmospheric carbon dioxide and weathering products in SNC meteorites

Other

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

86

Carbon Dioxide, Mars Atmosphere, Meteoritic Composition, Carbon Isotopes, Mass Spectroscopy, Weathering

Scientific paper

Stepped combustion analyses of SNC meteorites, which are postulated to have originated on Mars, are described. The results show that most of the carbon present in the samples can be ascribed to terrestrial contamination. EETA79001, however, contains 4.6 ppm of an isotropically distinct component enriched in C-13 (delta C-13 = +36 per mil), whereas high-temperature carbon of inferred igneous origin in this meteorite and other SNCs has a delta C-13 value of about -30 per mil. The C-12/C-13 ratio of the isotopically heavy component is within the error limits of Viking measurements in the Martian atmosphere, and thus strengthens the case for a planetary origin. Another carbon-containing species, believed to be carbonate, has been found in Nakhla (delta C-13 between +12 and +24 per mil) and may be a product of atmospheric weathering on Mars.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Martian atmospheric carbon dioxide and weathering products in SNC meteorites does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Martian atmospheric carbon dioxide and weathering products in SNC meteorites, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Martian atmospheric carbon dioxide and weathering products in SNC meteorites will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-825935

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.