Cryogenic Weathering as a Mechanism for Extreme 13C Enrichment in Martian Carbonate: Soil from Wright Valley, Antarctic as a Terrestrial Analog

Details Cryogenic Weathering as a Mechanism for Extreme 13C Enrichment in Martian Carbonate: Soil from Wright Valley, Antarctic as a Terrestrial Analog Cryogenic Weathering as a Mechanism for Extreme 13C Enrichment in Martian Carbonate: Soil from Wright Valley, Antarctic as a Terrestrial Analog

Mar 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995lpi....26.1333s&link_type=gif

Abstracts of the Lunar and Planetary Science Conference, volume 26, page 1333, (1995)

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