Did (some) carbonate & serpentine alteration of ultramafic rocks on Mars occur via ambient weathering over billions of years?

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    W[2022AGUFM.P52C1551L]
    LA["Linked Authors (4)"]
    LI["Linked Institutions (5)"]
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    W== affil ==>LI
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    click LI "#linked-institutions"
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ADS bibcode
2022AGUFM.P52C1551L
year
2022
Listed Authors
Leong, James Andrew Monton
Kelemen, Peter B.
Evans, Owen
Ghiorso, Mark S.
Mustard, John F.
Ehlmann, Bethany L.
Spiegelman, Marc W.
Debaille, Vinciane
Kaufman, Sierra
Listed Institutions
Lamont Doherty Earth Observatory, Columbia University, Palisades, United States
Lamont Doherty Earth Observatory, Columbia University, Palisades, United States
Columbia University, New York, United States
OFM Research, Redmond, United States
Brown University, Providence, United States
California Institute of Technology, Pasadena, United States
Columbia University, New York, United States
Université Libre de Bruxelles, Brussels, Belgium
Brown University, Providence, United States

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