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Le volcanisme carbonifère-supérieur du massif des grandes rousses (zone Dauphinoise - Alpes externes françaises) : un magmatisme affinites shoshonitiques lie a la fracturation crustale tardi-varisque

By: Contributor(s): Material type: ArticleArticleLanguage: Fre ISSN:
  • 03673685
Subject(s): Other classification:
  • Rev 530
 In: Géologie alpine 61, 1985, p. 33-60: : carte, graph., tab.
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bibliogr. p. 55-60

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