Puncturing Mars: How impact craters interact with the Martian cryosphere

Geologic evidence suggests that the Martian surface and atmospheric conditions underwent major changes in the late Noachian, with a decline in observable water-related surface features, suggestive of a transition to a dryer and colder climate. Based on that assumption, we have modeled the consequenc...

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Veröffentlicht in:Earth and planetary science letters 2012-06, Vol.335-336, p.9-17
Hauptverfasser: Schwenzer, S.P., Abramov, O., Allen, C.C., Clifford, S.M., Cockell, C.S., Filiberto, J., Kring, D.A., Lasue, J., McGovern, P.J., Newsom, H.E., Treiman, A.H., Vaniman, D.T., Wiens, R.C.
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Sprache:eng
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