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Buntsandstein unconformities and correlation in the western area of the triassic basin

dc.contributor.authorSánchez Moya, Yolanda
dc.contributor.authorMuñoz, A.
dc.contributor.authorRamos, A.
dc.contributor.authorSopeña, Alfonso
dc.description.abstractThe correlation among the diverse areas where the Triassic sediments have been described in the western Cordillera Ibérica and the border area of the Sistema Central has proved to show great difficulties. A very detailed field work, carried out here, have resulted in the elaboration ofa geological map where the various lithological units and the existing unconformities have been recognized A correlation chart has been elaborated where is clearly displayed how the main changes are related to the beginning of triassic where the major changes in thickness and facies took place, as a result of different subsidence areases_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherCordillera Ibérica-Sistema Centrales_ES
dc.titleLas discontinuidades estratigráficas del Buntsandstein en el borde occidental de la cuenca triásica y su implicación en las correlacioneses_ES
dc.titleBuntsandstein unconformities and correlation in the western area of the triassic basineng

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Atribución-NoComercial-SinDerivadas 3.0 España
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