Cooling of an early Earth magma ocean in interaction with the atmosphere

Abstract : We developed a 1D convective model of a cooling magma ocean that we coupled with a 1D radiativeconvective model of a primitive atmosphere [4]. Our main objective is to estimate the cooling time when the retroaction with the atmosphere is taken into account. We first describe our model and present some preliminary results of the coupled magma ocean / atmospheric model. We show that cooling time depends on the amount of volatiles released from the interior and is of order of 1 to 2 million years.
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https://hal.archives-ouvertes.fr/hal-00666263
Contributeur : Catherine Cardon <>
Soumis le : vendredi 3 février 2012 - 17:37:35
Dernière modification le : vendredi 16 novembre 2018 - 01:51:06

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T. Lebrun, H. Massol, Emmanuel Marcq, François Leblanc, G. Brandeis, et al.. Cooling of an early Earth magma ocean in interaction with the atmosphere. EPSC-DPS Joint Meeting 2011, Oct 2011, Nantes, France. 〈hal-00666263〉

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