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 |
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Sprache: | eng |
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