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Volumn 329, Issue 5997, 2010, Pages 1334-1337

Stable isotope measurements of martian atmospheric CO2 at the Phoenix landing site

Author keywords

[No Author keywords available]

Indexed keywords

CARBON; CARBON DIOXIDE; OXYGEN; SEA WATER; STABLE ISOTOPE; VOLATILE ORGANIC COMPOUND;

EID: 77956530124     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1192863     Document Type: Article
Times cited : (63)

References (33)
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    • note
    • 13C-enriched carbon is derived from a more ancient carbonate deposit that was incorporated into the younger nakhlites through dissolution and reprecipitation at the time of the Nakhla alteration event.
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    • note
    • We thank the members of the Mars Phoenix Project who enabled daily science operations at the Mars Phoenix landing site. We especially thank the Thermal and Evolved Gas Analyzer Science and Engineering Team, including H. Enos, G. Droege, C. Fellows, M. Finch, M. Fitzgibbon, and M. Williams. The Phoenix Mission was lead by the University of Arizona, Tucson, AZ, and was managed by NASA's Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA. The spacecraft was developed by Lockheed Martin Space Systems, Denver, CO. This paper benefited from two anonymous reviews and helpful discussions with J. Jones, E. Gibson, and R. Socki.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.