HIGHLIGHTS
- who: Chassefière E. et al. from the CNRS, Bât504, Orsay, France Tsinghua University have published the article: CO2-SO2 clathrate hydrate formation on early Mars, in the Journal: (JOURNAL)
- what: The authors propose here that the disruption may be due to the pressure decrease below 2 bar.
SUMMARY
The massive formation of sulfate minerals at the surface of Mars during the Hesperian could be the consequence of a drop of the CO2 pressure below a 2-bar threshold value at the late Noachian-Hesperian transition, which would have released . . .
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