Jagiellonian University Repository

Cretaceous (Aptian/Albian-?Cenomanian) age of "black flysch" and adjacent deposits of the Grajcarek thrust-sheets in the Małe Pieniny Mts. (Pieniny Klippen Belt, Polish Outer Carpathians)

Cretaceous (Aptian/Albian-?Cenomanian) age of "black ...

Show full item record

dc.contributor.author Oszczypko, Nestor [SAP11011866] pl
dc.contributor.author Olszewska, Barbara pl
dc.contributor.author Malata, Ewa [SAP11113447] pl
dc.date.accessioned 2016-08-18T11:33:30Z
dc.date.available 2016-08-18T11:33:30Z
dc.date.issued 2012 pl
dc.identifier.issn 1641-7291 pl
dc.identifier.uri http://ruj.uj.edu.pl/xmlui/handle/item/29702
dc.language eng pl
dc.rights Udzielam licencji. Uznanie autorstwa 3.0 Polska *
dc.rights.uri http://creativecommons.org/licenses/by/3.0/pl/legalcode *
dc.title Cretaceous (Aptian/Albian-?Cenomanian) age of "black flysch" and adjacent deposits of the Grajcarek thrust-sheets in the Małe Pieniny Mts. (Pieniny Klippen Belt, Polish Outer Carpathians) pl
dc.type JournalArticle pl
dc.description.physical 411-439 pl
dc.identifier.weblink https://gq.pgi.gov.pl/article/viewFile/7780 pl
dc.abstract.en Several sections record the relation between the "black flysch" and Upper Cretaceous red shales in the Grajcarek thrust-sheets. In all the sections studied the "black flysch" appears in the core of imbricated folds or thrust-sheets, whereas the limbs are composed of Upper Cretaceous deposits. The transitional beds between the "black flysch" and the Upper Cretaceous red shales are composed of green and black bituminous shales, green and red radiolarites and cherty limestones. Biostratigraphical investigations have revealed a similar type and sequence of microfauna assemblages in all the sections studied and significant redeposition of Jurassic calcareous benthic foraminifera, calcareous nannoplankton, molluscs, sponge spicules and crinoid elements. The Cretaceous age (Aptian/Albian-Cenomanian) of the "black flysch" is shown by the presence of agglutinated foraminifera and microfacies data. These deposits are underlain by a Kimmeridgian-Aptian radiolarite/limestone condensed succession and overlain by Turonian-Campanian hemipelagic red shales and Maastrichtian/Lower Paleocene conglomerates and thick-bedded silicilastic turbidites of the Jarmuta Formation. Such a sequence of deposits is typical of the Outer Carpathian basins and records the global Mid/Late Cretaceous phenomena in the world ocean, followed by the Cretaceous Oceanic Red Beds. pl
dc.subject.en "black flysch" pl
dc.subject.en Cretaceous pl
dc.subject.en foraminifera pl
dc.subject.en Pieniny Klippen Belt pl
dc.description.volume 56 pl
dc.description.number 3 pl
dc.identifier.doi 10.7306/gq.1031 pl
dc.identifier.eissn 2082-5099 pl
dc.title.journal Geological Quarterly pl
dc.language.container eng pl
dc.date.accession 2015-03-12 pl
dc.affiliation Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych pl
dc.subtype Article pl
dc.rights.original CC-BY; otwarte czasopismo; ostateczna wersja wydawcy; w momencie opublikowania; 0 pl
dc.identifier.project ROD UJ / P pl
.pointsMNiSW [2012 A]: 20


Files in this item

This item appears in the following Collection(s)

Udzielam licencji. Uznanie autorstwa 3.0 Polska Except where otherwise noted, this item's license is described as Udzielam licencji. Uznanie autorstwa 3.0 Polska