Contrasting tectonic styles of the western and eastern parts of the Western Carpathian Klippen Belt in Slovakia based on magnetotelluric sounding of deep tectonic structures

Bezák, Vladimír; Vozár, Ján; Majcin, Dušan; Klanica, Radek; Madarás, Ján

doi:10.7306/gq.1595

Artykuł - szczegóły

Tytuł artykułu

Contrasting tectonic styles of the western and eastern parts of the Western Carpathian Klippen Belt in Slovakia based on magnetotelluric sounding of deep tectonic structures

Autorzy

Bezák Vladimír , Vozár Ján , Majcin Dušan , Klanica Radek , Madarás Ján

Treść / Zawartość

Pełne teksty:

Bezak_V_Contrasting_GQ_Vol.65_No.2_2021.pdf

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Identyfikatory

DOI

10.7306/gq.1595

Warianty tytułu

Języki publikacji

Abstrakty

To characterize the deep structure of the Klippen Belt, we made magnetotelluric measurements in profiles across the western and eastern segments in the territory of Slovakia, from which we created 3D models. The models revealed significant differences in tectonic structure between these segments. In the western segment, the Klippen Belt is located in the southern reversing wing of the original subduction flower structure (retroarc thrusting) with an overthrust to the south onto the Inner Western Carpathian units. This structure was later modified by significant transpressional movements. In the eastern segment, the Klippen Belt is primarily an organic part of the accretionary wedge of the Outer Western Carpathians and it is overthrusted onto the Flysch Belt. This was followed by modification of the structures, mostly in a transpressional regime, including local reversing overthrusts and the development of a steep fault boundary, mainly along the southern margin, against the Inner Carpathian Paleogene succession. These differences between the structure of the western and eastern Klippen Belt segments indicate the contrast between the interaction of the western and eastern parts of the Inner Western Carpathians with the European Platform. In the western part, oblique collision and sinistral transpression dominate. In the eastern part, by contrast, subduction and orthogonal collision dominated over later transpressional modifications.

Słowa kluczowe

Western Carpathians Klippen Belt magnetotelluric sounding deep structures subduction collision transpression

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2021

Tom

Vol. 65, No. 2

Strony

art. no. 25

Opis fizyczny

Bibliogr. 94 poz., rys.

Twórcy

autor

Bezák Vladimír

geofbezv@savba.sk

Slovak Academy of Sciences, Earth Science Institute, Dúbravská 9, 840 05 Bratislava, Slovak Republic

autor

Vozár Ján

Slovak Academy of Sciences, Earth Science Institute, Dúbravská 9, 840 05 Bratislava, Slovak Republic

autor

Majcin Dušan

Slovak Academy of Sciences, Earth Science Institute, Dúbravská 9, 840 05 Bratislava, Slovak Republic

autor

Klanica Radek

Institute of Geophysics of the Czech Academy of Sciences, Boční II/1401, 141 31 Praha 4, Czech Republic

autor

Madarás Ján

Slovak Academy of Sciences, Earth Science Institute, Dúbravská 9, 840 05 Bratislava, Slovak Republic

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Opracowanie rekordu ze środków MNiSW, umowa Nr 461252 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2021).

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