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Updated: Jan 11, 2026

Simulation of Early Earth Hydrothermal Chimneys in a Thermal Gradient Environment
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火星の初期の地化学環境は,フィロシリケートの熱力学から決定された

Vincent Chevrier1, Francois Poulet, Jean-Pierre Bibring

  • 1W. M. Keck Laboratory for Space Simulation, Arkansas Center for Space and Planetary Sciences, MUSE 202, University of Arkansas, Fayetteville, Arkansas 72701, USA. vchevrie@uark.edu

Nature
|July 6, 2007
PubMed
まとめ

初期の火星は,二酸化炭素以外の温室効果ガスの影響により,液体の水が存在していたのかもしれません. フィロシリケート気象は,低レベルの二酸化炭素にもかかわらず,酸性条件ではなく,弱く酸性からアルカリ性のある環境を示唆しています.

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