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dc.contributor.authorReháková, Daniela
dc.contributor.authorŠulgan, František
dc.contributor.authorVašíček, Zdeněk
dc.contributor.authorMichalík, Jozef
dc.date.accessioned2007-10-22T11:01:12Z
dc.date.available2007-10-22T11:01:12Z
dc.date.issued1995
dc.identifier.citationGeologica Carpathica. 1995, vol. 46, no. 1, p. 53-58.en
dc.identifier.issn1335-0552
dc.identifier.issn1336-8052
dc.identifier.urihttp://hdl.handle.net/10084/63809
dc.language.isoenen
dc.publisherSlovak Academic Pressen
dc.relation.ispartofseriesGeologica Carpathicaen
dc.relation.urihttp://www.geologicacarpathica.sk/src/abstract.php?id=1995004600010053en
dc.subjectBerriasianen
dc.subjectLower Cretaceousen
dc.subjectOuter Carpathiansen
dc.subjectpelagic limestonesen
dc.subjectcalciturbiditesen
dc.subjectcalpionellidsen
dc.subjectcalcareous dinoflagellatesen
dc.subjectaptychien
dc.titleEnvironment, fauna and paleogeographic importance of the berriasian limestones from the Vigantice tectonic slice in the Outer Western Carpathiansen
dc.typearticleen
dc.identifier.locationVe fondu ÚKen
dc.description.abstract-enThe limestones of the Vigantice tectonic slice represent one of the few preserved remnants of the sedimentary record of Mesozoic sedimentation in the Cetechovice Basin of the Outer Carpathians. The sequences of pelagic limestones contain calciturbidite intercalations with clastic material originating from the Silesian cordillera. The fauna of aptychi (Punctaptychus punctatus punctatus, P. p. rectecostatus, P. sp., Lamellaptychus beyrichi beyrichi, L. submortilleti) indicates a Berriasian age of the limestones. The association of calpionellids is typical of the Calpionella Zone.en
dc.identifier.wosA1995QX85100007


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