Stages of development in the Polish Carpathian Foredeep basin

2012
journal article
article
50
dc.abstract.enIn southern Poland, Miocene deposits have been recognised both in the Outer Carpathians and the Carpathian Foredeep (PCF). In the Outer Carpathians, the Early Miocene deposits represent the youngest part of the flysch sequence, while in the Polish Carpathian Foredeep they are developed on the basement platform. The inner foredeep (beneath the Carpathians) is composed of Early to Middle Miocene deposits, while the outer foredeep is filled up with the Middle Miocene (Badenian and Sarmatian) strata, up to 3,000mthick. The Early Miocene strata are mainly terrestrial in origin, whereas the Badenian and Sarmatian strata are marine. The Carpathian Foredeep developed as a peripheral foreland basin related to the moving Carpathian front. The main episodes of intensive subsidence in the PCF correspond to the period of progressive emplacement of the Western Carpathians onto the foreland plate. The important driving force of tectonic subsidence was the emplacement of the nappe load related to subduction roll-back. During that time the loading effect of the thickening of the Carpathian accretionary wedge on the foreland plate increased and was followed by progressive acceleration of total subsidence. The mean rate of the Carpathian overthrusting, and north to north-east migration of the axes of depocentres reached 12 mm/yr at that time. During the Late Badenian-Sarmatian, the rate of advance of the Carpathian accretionary wedge was lower than that of pinch-out migration and, as a result, the basin widened. The Miocene convergence of the Carpathian wedge resulted in the migration of depocentres and onlap of successively younger deposits onto the foreland plate.pl
dc.affiliationWydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznychpl
dc.contributor.authorOszczypko, Nestor - 131218 pl
dc.contributor.authorOszczypko-Clowes, Marta - 131219 pl
dc.date.accession2015-04-02pl
dc.date.accessioned2016-06-03T12:20:31Z
dc.date.available2016-06-03T12:20:31Z
dc.date.issued2012pl
dc.date.openaccess0
dc.description.accesstimew momencie opublikowania
dc.description.number1pl
dc.description.physical138-162pl
dc.description.versionostateczna wersja wydawcy
dc.description.volume4pl
dc.identifier.doi10.2478/s13533-011-0044-0pl
dc.identifier.eissn1896-1517pl
dc.identifier.issn2081-9900pl
dc.identifier.projectROD UJ / Ppl
dc.identifier.urihttp://ruj.uj.edu.pl/xmlui/handle/item/27448
dc.identifier.weblinkhttp://link.springer.com/article/10.2478/s13533-011-0044-0pl
dc.languageengpl
dc.language.containerengpl
dc.rightsUdzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0*
dc.rights.licenceCC-BY
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/legalcode*
dc.share.typeinne
dc.subject.enPolish Carpathian Foredeeppl
dc.subject.enpalaeogeographypl
dc.subject.ennannofossil biostratigraphypl
dc.subject.enbasin evolutionpl
dc.subtypeArticlepl
dc.titleStages of development in the Polish Carpathian Foredeep basinpl
dc.title.journalCentral European Journal of Geosciencespl
dc.typeJournalArticlepl
dspace.entity.typePublication
dc.abstract.enpl
In southern Poland, Miocene deposits have been recognised both in the Outer Carpathians and the Carpathian Foredeep (PCF). In the Outer Carpathians, the Early Miocene deposits represent the youngest part of the flysch sequence, while in the Polish Carpathian Foredeep they are developed on the basement platform. The inner foredeep (beneath the Carpathians) is composed of Early to Middle Miocene deposits, while the outer foredeep is filled up with the Middle Miocene (Badenian and Sarmatian) strata, up to 3,000mthick. The Early Miocene strata are mainly terrestrial in origin, whereas the Badenian and Sarmatian strata are marine. The Carpathian Foredeep developed as a peripheral foreland basin related to the moving Carpathian front. The main episodes of intensive subsidence in the PCF correspond to the period of progressive emplacement of the Western Carpathians onto the foreland plate. The important driving force of tectonic subsidence was the emplacement of the nappe load related to subduction roll-back. During that time the loading effect of the thickening of the Carpathian accretionary wedge on the foreland plate increased and was followed by progressive acceleration of total subsidence. The mean rate of the Carpathian overthrusting, and north to north-east migration of the axes of depocentres reached 12 mm/yr at that time. During the Late Badenian-Sarmatian, the rate of advance of the Carpathian accretionary wedge was lower than that of pinch-out migration and, as a result, the basin widened. The Miocene convergence of the Carpathian wedge resulted in the migration of depocentres and onlap of successively younger deposits onto the foreland plate.
dc.affiliationpl
Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych
dc.contributor.authorpl
Oszczypko, Nestor - 131218
dc.contributor.authorpl
Oszczypko-Clowes, Marta - 131219
dc.date.accessionpl
2015-04-02
dc.date.accessioned
2016-06-03T12:20:31Z
dc.date.available
2016-06-03T12:20:31Z
dc.date.issuedpl
2012
dc.date.openaccess
0
dc.description.accesstime
w momencie opublikowania
dc.description.numberpl
1
dc.description.physicalpl
138-162
dc.description.version
ostateczna wersja wydawcy
dc.description.volumepl
4
dc.identifier.doipl
10.2478/s13533-011-0044-0
dc.identifier.eissnpl
1896-1517
dc.identifier.issnpl
2081-9900
dc.identifier.projectpl
ROD UJ / P
dc.identifier.uri
http://ruj.uj.edu.pl/xmlui/handle/item/27448
dc.identifier.weblinkpl
http://link.springer.com/article/10.2478/s13533-011-0044-0
dc.languagepl
eng
dc.language.containerpl
eng
dc.rights*
Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0
dc.rights.licence
CC-BY
dc.rights.uri*
http://creativecommons.org/licenses/by-nc-nd/3.0/legalcode
dc.share.type
inne
dc.subject.enpl
Polish Carpathian Foredeep
dc.subject.enpl
palaeogeography
dc.subject.enpl
nannofossil biostratigraphy
dc.subject.enpl
basin evolution
dc.subtypepl
Article
dc.titlepl
Stages of development in the Polish Carpathian Foredeep basin
dc.title.journalpl
Central European Journal of Geosciences
dc.typepl
JournalArticle
dspace.entity.type
Publication
Affiliations

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