The Noachian-Hesperian Transition on Mars: Geological Evidence for a Punctuated Phase of Global Volcanism as a Key Driver in Climate and Atmospheric Evolution

Physics

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Scientific paper

Early Hesperian peak volcanic flux caused short-term atmospheric warming
and led to basal melting of the south polar cap, formation of lower
latitude valley networks and open-basin lakes, and a transition to
sulfur-dominated weathering.

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