LOWER PALEOZOIC ISOPIC ZONES OF NORTHWESTERN MEXICO AS EVIDENCE OF CONTINUITY BETWEEN APPALACHIAN MOUNTAINS AND WEST AMERICAN CORDILLERA

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dc.contributor.authorPEIFFERRANGIN, F
dc.date.accessioned2026-05-28T16:30:17Z
dc.date.issued1970
dc.description.paginacion1517 - 1519
dc.description.procedenciaEXT
dc.format.discursoArtículo
dc.format.extent3
dc.identifier.issn0567-655X
dc.identifier.urihttps://ahcm.cinvestav.mx/handle/ahcm/22776
dc.language.isoFrancés
dc.numero.secuencia22773
dc.publisherUNIV PARIS 06, GEOL STRUCT LAB, F-75230 PARIS 05, FRANCE
dc.relation.ispartofseriesVol. 288 No. 20
dc.source.revistafuenteCOMPTES RENDUS HEBDOMADAIRES DES SEANCES DE L ACADEMIE DES SCIENCES SERIE D
dc.subjectPALEOZOIC, ISOPIC, MEXICO, MOUNTAINS, AMERICAN, CORDILLERA
dc.subject.categoriaprincipalMULTIDISCIPLINARIA
dc.subject.disciplinaGEOLOGIA
dc.subject.subdisciplinaESTRATIGRAFIA
dc.titleLOWER PALEOZOIC ISOPIC ZONES OF NORTHWESTERN MEXICO AS EVIDENCE OF CONTINUITY BETWEEN APPALACHIAN MOUNTAINS AND WEST AMERICAN CORDILLERA
dc.title.alternativeCOM REN HEBD SEAN ACAD SCI SERIE D

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