Biblioteca IFEA
Biblioteca IFEA
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Ollantaytambo formation : a probably arc-derived volcaniclastic succession of cambrian to ordovician age in the Cordillera Oriental of southern Peru

By: Contributor(s): Material type: ArticleArticleLanguage: Eng Other classification:
  • Am.Géol 306a
 In: Géodynamique andine : résumés étendusAndean geodynamics : extended abstractsGeodinámica andina : resúmenes ampliados p. 69-71
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bibliogr. p. 71

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