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Les ophiolites helleniques pelagoniennes charriées au jurassique supérieur proviennent-elles d'une mer marginale au d'un océan du vardar

By: Contributor(s): Material type: ArticleArticleLanguage: Fre Subject(s): Other classification:
  • Géol 191b
 In: 3° réunion annuelle des sciences de la terre p. 262 : ill.
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