Publication:
Vendian-Cambrian of Western Gondwana: Introduction

dc.creatorGaucher, Claudio
dc.creatorFrimmel, Hartwig E.
dc.creatorFerreira, Valderez P.
dc.creatorPoire, Daniel Gustavo
dc.date.issued2004-12
dc.description.abstractGondwana (Suess, 1875) formed as a result of the Pan African-Brasiliano orogenies, and survived until the opening of the Atlantic in late Mesozoic times. For researchers dealing with the genesis of this remarkable supercontinent, the time period represented by the Vendian to Cambrian (ca. 600-500 Ma) is crucial.
dc.identifierGaucher, Claudio; Frimmel, Hartwig E.; Ferreira, Valderez P.; Poire, Daniel Gustavo; Vendian-Cambrian of Western Gondwana: Introduction; Elsevier Science; Gondwana Research; 7; 3; 12-2004; 659-660
dc.identifier1342-937X
dc.identifierhttp://hdl.handle.net/11336/75927
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://naturalis.fcnym.unlp.edu.ar/handle/628872547/57746
dc.languageeng
dc.publisherElsevier Science
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1342937X05710534
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/https://doi.org/10.1016/S1342-937X(05)71053-4
dc.subjectVendian-Cambrian
dc.subjectSouth-Western Gondwana
dc.subjectPalaeogeography
dc.subjectIgcp 478
dc.titleVendian-Cambrian of Western Gondwana: Introduction
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:ar-repo/semantics/artículo
dc.typeinfo:eu-repo/semantics/publishedVersion
dspace.entity.typePublication

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