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Preliminary study about the volcaniclastic facies in the Zamoranos Formation (Subbetic Triassic)

dc.contributor.authorPérez López, Alberto
dc.contributor.authorMorata Céspedes, Diego
dc.date.accessioned2017-08-11T11:32:00Z
dc.date.available2017-08-11T11:32:00Z
dc.date.issued1993
dc.identifier.urihttp://hdl.handle.net/10272/14034
dc.description.abstractIn some outcrops o f the Trias o f facies Keuper in the Central Subbetic Zone has been defined the Zamorano Formation, dated as Norian. In this formation is possible to identify conglomerates with pebbles of different nature, between them, the volcanogenetic ones. These last are present as porphyritic basaltic and glasses fragments. These volcaniclastic rocks have been interpreted as the result of a pre-or Norian volcanic activity in the south Iberian Triassic shelfes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherSubbetices_ES
dc.subject.otherTriassices_ES
dc.subject.otherNorianes_ES
dc.subject.otherVolcaniclastic facieses_ES
dc.subject.otherBasaltes_ES
dc.titleEstudio preliminar sobre las facies volcaníclásticas de la Formación Zamoranos (Trías Subbético)es_ES
dc.titlePreliminary study about the volcaniclastic facies in the Zamoranos Formation (Subbetic Triassic)eng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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