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The Lower Miocene deposits of the Rača Subunit near Nowy Sącz (Magura Nappe, Polish outer Carpathians)

1999
journal article
article
Journal
Geologica Carpathica
Author
Oszczypko Nestor

Andreyeva-Grigorovich Aida S.

Malata Ewa

Oszczypko-Clowes Marta
Volume
50
Number
6
Pages
419-433
ISSN
1335-0552
eISSN
1336-8052
Keywords in English

Lower Miocene

Outer Carpathians

Magura Nappe

Rača Subunit

lithostratigraphy

calcareous nannoplankton

foraminifers

paleogeography

URL
https://geologicacarpathica.com/browse/archive/?journal_article_no=2543
Access date
2025-11-17
Remarks

Bibliogr. s. 432-433

Language
English
Journal language
English
Abstract in English

In the area of Nowy Sącz the Lower Miocene, marine deposits (of the N 5, NN 2-3 biozones) have been discovered in the southern part of the Rača Subunit of the Magura Nappe. These deposits belong to the Zawada Fm., which probably overlaps the Malcov Fm. (Upper Eocene-Oligocene) with an erosional hiatus. These folded deposits are represented by medium- to thick-bedded glauconitic sandstones with intercalations of thick-bedded marls. Facies-lithological development of the Zawada Fm. displays features characteristic for the northern part of the Magura Basin (Siary facies zone). During the Early Burdigalian the partly folded Magura Nappe was flooded from the residual flysch basin located in the north. At that time the seaway connection between this basin and the Vienna Basin via the Orava area was probable established.

Affiliation
Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych
dc.abstract.enIn the area of Nowy Sącz the Lower Miocene, marine deposits (of the N 5, NN 2-3 biozones) have been discovered in the southern part of the Rača Subunit of the Magura Nappe. These deposits belong to the Zawada Fm., which probably overlaps the Malcov Fm. (Upper Eocene-Oligocene) with an erosional hiatus. These folded deposits are represented by medium- to thick-bedded glauconitic sandstones with intercalations of thick-bedded marls. Facies-lithological development of the Zawada Fm. displays features characteristic for the northern part of the Magura Basin (Siary facies zone). During the Early Burdigalian the partly folded Magura Nappe was flooded from the residual flysch basin located in the north. At that time the seaway connection between this basin and the Vienna Basin via the Orava area was probable established.pl
dc.affiliationWydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznychpl
dc.contributor.authorOszczypko, Nestor - 131218 pl
dc.contributor.authorAndreyeva-Grigorovich, Aida S.pl
dc.contributor.authorMalata, Ewa - 102578 pl
dc.contributor.authorOszczypko-Clowes, Marta - 131219 pl
dc.date.accession2025-11-17
dc.date.accessioned2018-10-10T12:58:16Z
dc.date.available2018-10-10T12:58:16Z
dc.date.issued1999pl
dc.date.openaccess0
dc.description.accesstimew momencie opublikowania
dc.description.additionalBibliogr. s. 432-433pl
dc.description.number6pl
dc.description.physical419-433pl
dc.description.publication2,2pl
dc.description.versionostateczna wersja wydawcy
dc.description.volume50pl
dc.identifier.eissn1336-8052pl
dc.identifier.issn1335-0552pl
dc.identifier.projectDRC AI
dc.identifier.urihttps://ruj.uj.edu.pl/xmlui/handle/item/57799
dc.identifier.weblinkhttps://geologicacarpathica.com/browse/archive/?journal_article_no=2543
dc.languageengpl
dc.language.containerengpl
dc.rightsUdzielam licencji. Uznanie 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.pl
dc.share.typeotwarte czasopismo
dc.source.integratorfalse
dc.subject.enLower Miocenepl
dc.subject.enOuter Carpathianspl
dc.subject.enMagura Nappepl
dc.subject.enRača Subunitpl
dc.subject.enlithostratigraphypl
dc.subject.encalcareous nannoplanktonpl
dc.subject.enforaminiferspl
dc.subject.enpaleogeographypl
dc.subtypeArticlepl
dc.titleThe Lower Miocene deposits of the Rača Subunit near Nowy Sącz (Magura Nappe, Polish outer Carpathians)pl
dc.title.journalGeologica Carpathicapl
dc.typeJournalArticlepl
dspace.entity.typePublication
dc.abstract.enpl
In the area of Nowy Sącz the Lower Miocene, marine deposits (of the N 5, NN 2-3 biozones) have been discovered in the southern part of the Rača Subunit of the Magura Nappe. These deposits belong to the Zawada Fm., which probably overlaps the Malcov Fm. (Upper Eocene-Oligocene) with an erosional hiatus. These folded deposits are represented by medium- to thick-bedded glauconitic sandstones with intercalations of thick-bedded marls. Facies-lithological development of the Zawada Fm. displays features characteristic for the northern part of the Magura Basin (Siary facies zone). During the Early Burdigalian the partly folded Magura Nappe was flooded from the residual flysch basin located in the north. At that time the seaway connection between this basin and the Vienna Basin via the Orava area was probable established.
dc.affiliationpl
Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych
dc.contributor.authorpl
Oszczypko, Nestor - 131218
dc.contributor.authorpl
Andreyeva-Grigorovich, Aida S.
dc.contributor.authorpl
Malata, Ewa - 102578
dc.contributor.authorpl
Oszczypko-Clowes, Marta - 131219
dc.date.accession
2025-11-17
dc.date.accessioned
2018-10-10T12:58:16Z
dc.date.available
2018-10-10T12:58:16Z
dc.date.issuedpl
1999
dc.date.openaccess
0
dc.description.accesstime
w momencie opublikowania
dc.description.additionalpl
Bibliogr. s. 432-433
dc.description.numberpl
6
dc.description.physicalpl
419-433
dc.description.publicationpl
2,2
dc.description.version
ostateczna wersja wydawcy
dc.description.volumepl
50
dc.identifier.eissnpl
1336-8052
dc.identifier.issnpl
1335-0552
dc.identifier.project
DRC AI
dc.identifier.uri
https://ruj.uj.edu.pl/xmlui/handle/item/57799
dc.identifier.weblink
https://geologicacarpathica.com/browse/archive/?journal_article_no=2543
dc.languagepl
eng
dc.language.containerpl
eng
dc.rights
Udzielam licencji. 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.pl
dc.share.type
otwarte czasopismo
dc.source.integrator
false
dc.subject.enpl
Lower Miocene
dc.subject.enpl
Outer Carpathians
dc.subject.enpl
Magura Nappe
dc.subject.enpl
Rača Subunit
dc.subject.enpl
lithostratigraphy
dc.subject.enpl
calcareous nannoplankton
dc.subject.enpl
foraminifers
dc.subject.enpl
paleogeography
dc.subtypepl
Article
dc.titlepl
The Lower Miocene deposits of the Rača Subunit near Nowy Sącz (Magura Nappe, Polish outer Carpathians)
dc.title.journalpl
Geologica Carpathica
dc.typepl
JournalArticle
dspace.entity.type
Publication
Affiliations
No affiliation
Oszczypko, Nestor
Andreyeva-Grigorovich, Aida S.
Malata, Ewa
Oszczypko-Clowes, Marta

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