Jurassic paleogeography of the Pieniny and Outer Carpathian basins

2004
journal article
article
cris.lastimport.wos2024-04-09T20:35:54Z
dc.abstract.enThe Jurassic history of the Pieniny/Outer Carpathian basins reflects the evolution of the Circum-Tethyan area, especially its Alpine Tethys part. The Alpine Tethys that is Ligurian, Penninic Oceans and Pieniny/Magura Basin constitute the extension of the Central Atlantic system. The synrift stage lasted in the Pieniny/Magura Basin from late Early Jurassic to Tithonian (the Magura Unit constitutes the southernmost part of the Outer Flysch Carpathians). The Pieniny rift opened during Pliensbachian - Aalenian. The central Atlantic and Alpine Tethys went into a drifting stage during the Middle Jurassic. The Late Jurassic (Oxfordian-Kimmeridgian) history of the Pieniny/Magura Basin reflects strongest facial differentiation within sedimentary basin where mixed siliceous-carbonate sedimentation took place. Greatest deepening effect is indicated by widespread Oxfordian radiolarites, which occur in the all basinal successions, whereas the shallowest zone is completely devoid of siliceous intercalations at that time (sedimentation from Ammonitico Rosso facies up to coral reef limestone). The southern part of the North European Platform, north from the Pieniny/Magura realm, started to be rifted during Late Jurassic time and Silesian Basin in the Outer Western Carpathians and Sinaia Basin in the Eastern Carpathians, with black, mainly redeposited marls have been created. The outer sub-basins were differentiated during the latest (Hauterivian-Barremian) phase of basinal development. The connection of Silesian Basin with Sinaia and Southern Carpathian Severin areas suggests the NW-SE direction of the basinal axis while the orientation of the Pieniny Klippen Belt/Magura Basin was SW-NE so, two Outer Carpathian perpendicular directions are possible within the basins. Major reorganization happened during the Tithonian-Berriasian time. It was reflected by both paleoceanographical and paleoclimatical changes. The Neo-Cimmerian tectonic events as well as main phase of the Outer Carpathian basins opening is connected with this reorganization.pl
dc.affiliationWydział Biologii i Nauk o Ziemipl
dc.contributor.authorGolonka, Janpl
dc.contributor.authorKrobicki, Michałpl
dc.date.accessioned2018-10-31T13:42:17Z
dc.date.available2018-10-31T13:42:17Z
dc.date.issued2004pl
dc.date.openaccess0
dc.description.accesstimew momencie opublikowania
dc.description.additionalBibliogr. s. 13-14pl
dc.description.number1pl
dc.description.physical5-14pl
dc.description.versionostateczna wersja wydawcy
dc.description.volume110pl
dc.identifier.doi10.13130/2039-4942/6252pl
dc.identifier.eissn2039-4942pl
dc.identifier.issn0035-6883pl
dc.identifier.projectROD UJ / OPpl
dc.identifier.urihttps://ruj.uj.edu.pl/xmlui/handle/item/59193
dc.languageengpl
dc.language.containerengpl
dc.rightsUznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 4.0 Międzynarodowa*
dc.rights.licenceCC-BY-NC-ND
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/legalcode*
dc.share.typeotwarte czasopismo
dc.subject.enJurassicpl
dc.subject.enCarpathianspl
dc.subject.enTethyspl
dc.subject.enplate tectonicspl
dc.subject.enpaleogeographypl
dc.subtypeArticlepl
dc.titleJurassic paleogeography of the Pieniny and Outer Carpathian basinspl
dc.title.journalRivista Italiana di Paleontologia e Stratigrafiapl
dc.typeJournalArticlepl
dspace.entity.typePublication
cris.lastimport.wos
2024-04-09T20:35:54Z
dc.abstract.enpl
The Jurassic history of the Pieniny/Outer Carpathian basins reflects the evolution of the Circum-Tethyan area, especially its Alpine Tethys part. The Alpine Tethys that is Ligurian, Penninic Oceans and Pieniny/Magura Basin constitute the extension of the Central Atlantic system. The synrift stage lasted in the Pieniny/Magura Basin from late Early Jurassic to Tithonian (the Magura Unit constitutes the southernmost part of the Outer Flysch Carpathians). The Pieniny rift opened during Pliensbachian - Aalenian. The central Atlantic and Alpine Tethys went into a drifting stage during the Middle Jurassic. The Late Jurassic (Oxfordian-Kimmeridgian) history of the Pieniny/Magura Basin reflects strongest facial differentiation within sedimentary basin where mixed siliceous-carbonate sedimentation took place. Greatest deepening effect is indicated by widespread Oxfordian radiolarites, which occur in the all basinal successions, whereas the shallowest zone is completely devoid of siliceous intercalations at that time (sedimentation from Ammonitico Rosso facies up to coral reef limestone). The southern part of the North European Platform, north from the Pieniny/Magura realm, started to be rifted during Late Jurassic time and Silesian Basin in the Outer Western Carpathians and Sinaia Basin in the Eastern Carpathians, with black, mainly redeposited marls have been created. The outer sub-basins were differentiated during the latest (Hauterivian-Barremian) phase of basinal development. The connection of Silesian Basin with Sinaia and Southern Carpathian Severin areas suggests the NW-SE direction of the basinal axis while the orientation of the Pieniny Klippen Belt/Magura Basin was SW-NE so, two Outer Carpathian perpendicular directions are possible within the basins. Major reorganization happened during the Tithonian-Berriasian time. It was reflected by both paleoceanographical and paleoclimatical changes. The Neo-Cimmerian tectonic events as well as main phase of the Outer Carpathian basins opening is connected with this reorganization.
dc.affiliationpl
Wydział Biologii i Nauk o Ziemi
dc.contributor.authorpl
Golonka, Jan
dc.contributor.authorpl
Krobicki, Michał
dc.date.accessioned
2018-10-31T13:42:17Z
dc.date.available
2018-10-31T13:42:17Z
dc.date.issuedpl
2004
dc.date.openaccess
0
dc.description.accesstime
w momencie opublikowania
dc.description.additionalpl
Bibliogr. s. 13-14
dc.description.numberpl
1
dc.description.physicalpl
5-14
dc.description.version
ostateczna wersja wydawcy
dc.description.volumepl
110
dc.identifier.doipl
10.13130/2039-4942/6252
dc.identifier.eissnpl
2039-4942
dc.identifier.issnpl
0035-6883
dc.identifier.projectpl
ROD UJ / OP
dc.identifier.uri
https://ruj.uj.edu.pl/xmlui/handle/item/59193
dc.languagepl
eng
dc.language.containerpl
eng
dc.rights*
Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 4.0 Międzynarodowa
dc.rights.licence
CC-BY-NC-ND
dc.rights.uri*
http://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
dc.share.type
otwarte czasopismo
dc.subject.enpl
Jurassic
dc.subject.enpl
Carpathians
dc.subject.enpl
Tethys
dc.subject.enpl
plate tectonics
dc.subject.enpl
paleogeography
dc.subtypepl
Article
dc.titlepl
Jurassic paleogeography of the Pieniny and Outer Carpathian basins
dc.title.journalpl
Rivista Italiana di Paleontologia e Stratigrafia
dc.typepl
JournalArticle
dspace.entity.type
Publication
Affiliations

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