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Identificación orbital de las rocas carbonatadas en Marte

Bethany L Ehlmann1, John F Mustard, Scott L Murchie

  • 1Department of Geological Sciences, Brown University, Providence, RI02912, USA.

Science (New York, N.Y.)
|December 20, 2008
PubMed
Resumen

Las rocas de carbonato de magnesio detectadas en Marte sugieren condiciones de agua pasadas de neutrales a alcalinas. Este descubrimiento desafía la idea de que el clima ácido dominó todos los ambientes marcianos antiguos.

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