The intramontane Orava Basin - evidence of large-scale Miocene to Quaternary sinistral wrenching in the Alpine-Carpathian-Pannonian area

Ludwiniak, Mirosław; Śmigielski, Michał; Kowalczyk, Sebastian; Łoziński, Maciej; Czarniecka, Urszula; Lewińska, Lena

doi:10.24425/agp.2019.126449

Artykuł - szczegóły

Tytuł artykułu

The intramontane Orava Basin - evidence of large-scale Miocene to Quaternary sinistral wrenching in the Alpine-Carpathian-Pannonian area

Autorzy

Ludwiniak Mirosław , Śmigielski Michał , Kowalczyk Sebastian , Łoziński Maciej , Czarniecka Urszula , Lewińska Lena

Treść / Zawartość

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Identyfikatory

DOI

10.24425/agp.2019.126449

Warianty tytułu

Języki publikacji

Abstrakty

The Carpathian Orava Basin is a tectonic structure filled with Neogene and Quaternary deposits superimposed on the collision zone between the ALCAPA and European plates. Tectonic features of the south-eastern margin of the Orava Basin and the adjoining part of the fore-arc Central Carpathian Palaeogene Basin were studied. Field observations of mesoscopic structures, analyses of digital elevation models and geological maps, supplemented with electrical resistivity tomography surveys were performed. Particular attention was paid to joint network analysis. The NE-SW-trending Krowiarki and Hruštinka-Biela Orava sinistral fault zones were recognized as key tectonic features that influenced the Orava Basin development. They constitute the north-eastern part of a larger Mur-Mürz-Žilina fault system that separates the Western Carpathians from the Eastern Alps. The interaction of these sinistral fault zones with the older tectonic structures of the collision zone caused the initiation and further development of the Orava Basin as a strike-slip-related basin. The Krowiarki Fault Zone subdivides areas with a different deformation pattern within the sediments of the Central Carpathian Palaeogene Basin and was active at least from the time of cessation of its sedimentation in the early Miocene. Comparison of structural data with the recent tectonic stress field, earthquake focal mechanisms and GPS measurements allows us to conclude that the Krowiarki Fault Zone shows a stable general pattern of tectonic activity for more than the last 20 myr and is presently still active.

Słowa kluczowe

Orava Basin Central Carpathian Palaeogene Basin structural analysis strike-slip related basin transrotational basin joint pattern analysis Western Carpathians

Kotlina Orawska paleogeński basen centralno-karpacki paleogeńskiego basen Karpat centralnych analiza strukturalna basen przesuwczy basen transrotacyjny Karpaty Zachodnie

Wydawca

Faculty of Geology of the University of Warsaw
Komitet Nauk Geologicznych PAN

Czasopismo

Acta Geologica Polonica

Rocznik

2019

Tom

Vol. 69, no. 3

Strony

339--386

Opis fizyczny

Bibliogr. 222 poz., rys., tab., wykr.

Twórcy

autor

Ludwiniak Mirosław

Miroslaw.Ludwiniak@uw.edu.pl

Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warsaw, Poland

autor

Śmigielski Michał

Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warsaw, Poland

autor

Kowalczyk Sebastian

Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warsaw, Poland

autor

Łoziński Maciej

Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warsaw, Poland

autor

Czarniecka Urszula

Department of Geosciences, University of Oslo, P.O. Box 1047 Blindern, 0316 Oslo, Norway

autor

Lewińska Lena

Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warsaw, Poland

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2019).

Typ dokumentu

Bibliografia

Identyfikator YADDA

bwmeta1.element.baztech-b022cac4-4c7c-46ef-9b73-d831ea254318