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Utilisation de la reaction SiO2 + 2MnO = Mn2SiO4 pour determiner le coefficient de diffusion de la silice dans l'eau supercritique au dessous de 500° C

By: Contributor(s): Material type: ArticleArticleLanguage: Fre Other classification:
  • Géol 191d
 In: 5° Réunion annuelle des sciences de la terre p. 277
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