The relative influence of H2 O and CO2 on the primitive surface conditions and evolution of rocky planets
Author:
Affiliation:
1. FAST, CNRS; Univ. Paris-Sud, Université Paris-Saclay; Orsay France
2. GEOPS, CNRS; Univ. Paris-Sud, Université Paris-Saclay; Orsay France
3. LATMOS/IPSL, UVSQ; Université Paris-Saclay; Guyancourt France
Funder
CNRS-INSU-CNES national planetology program (PNP)
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017JE005286/fullpdf
Reference104 articles.
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3. The formation of an impact-generated H2O atmosphere and its implications for the early thermal history of the Earth;Abe;J. Geophys. Res.,1985
4. Evolution of an impact-generated H2O-CO2 atmosphere and formation of a hot proto-ocean on Earth;Abe;J. Atmos. Sci.,1988
5. Habitable zone limits for dry planets;Abe;Astrobiology,2011
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