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dc.contributor.authorMichalík, Jozef
dc.contributor.authorReháková, Daniela
dc.contributor.authorVašíček, Zdeněk
dc.date.accessioned2007-10-22T10:49:19Z
dc.date.available2007-10-22T10:49:19Z
dc.date.issued1995
dc.identifier.citationGeologica Carpathica. 1995, vol. 46, no. 5, p. 285-296.en
dc.identifier.issn1335-0552
dc.identifier.issn1336-8052
dc.identifier.urihttp://hdl.handle.net/10084/63807
dc.language.isoenen
dc.publisherSlovak Academic Pressen
dc.relation.ispartofseriesGeologica Carpathicaen
dc.relation.urihttp://www.geologicacarpathica.sk/src/abstract.php?id=1995004600050285en
dc.subjectLate Jurassic/Early Cretaceousen
dc.subjectWestern Carpathiansen
dc.subjectbasin evolutionen
dc.subjectcarbonate sedimentsen
dc.subjectbrecciasen
dc.subjectmicroplanktonen
dc.subjectammonitesen
dc.titleEarly cretaceous sedimentary changes in West-Carpathian areaen
dc.typearticleen
dc.identifier.locationVe fondu ÚKen
dc.description.abstract-enLatest Tithonian bottom relief denivelization, local erosion, as well as successive origin of Berriasian/Valanginian carbonate breccias influenced the sedimentary regime of the carbonate basins in Central Western Carpathians. The Nozdrovice Breccia is interpreted here as the product of sedimentation below an active fault slope. The distribution and composition of clastic intercalations in hemipelagic carbonate sequences indicate the dynamics of these basins during the Jurassic/Cretaceous transition.en
dc.identifier.wosA1995TL89100005


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