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Les gneiss acides à grenat-cordierite du Tormes, temoin de l'évolution du métamorphisme hercynien dans le centre-ouest de la Péninsule ibérique

By: Contributor(s): Material type: ArticleArticleLanguage: Fre Other classification:
  • Géol 191d
 In: 5° Réunion annuelle des sciences de la terre p. 246
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