Together but separate: decoupled Variscan (late Carboniferous) and Alpine (Late Cretaceous–Paleogene) inversion tectonics in NW Poland

In Europe, formation of the Palaeozoic Variscan orogenic belt, and the Mesozoic–Cenozoic Alpine–Carpathian orogenic belt led to a widespread inversion events within forelands of both orogenic domains. We used legacy 2-D seismic data together with the newly acquired 3-D seismic data that, for the fir...

Full description

Saved in:
Bibliographic Details
Published inSolid earth (Göttingen) Vol. 13; no. 3; pp. 639 - 658
Main Authors Krzywiec, Piotr, Kufrasa, Mateusz, Poprawa, Paweł, Mazur, Stanisław, Koperska, Małgorzata, Ślemp, Piotr
Format Journal Article
LanguageEnglish
Published Gottingen Copernicus GmbH 18.03.2022
Copernicus Publications
Subjects
Basins
Belts
Carboniferous
Cenozoic
Cretaceous
Data acquisition
Devonian
Earth science
Evaporites
Fault lines
Inversion
Mesozoic
Multilayers
Orogeny
Palaeozoic
Paleogene
Paleozoic
Plate tectonics
Seismic data
Subsidence
Tectonics
Two dimensional models
Poland
Online AccessGet full text

Cover

More Information
Summary:In Europe, formation of the Palaeozoic Variscan orogenic belt, and the Mesozoic–Cenozoic Alpine–Carpathian orogenic belt led to a widespread inversion events within forelands of both orogenic domains. We used legacy 2-D seismic data together with the newly acquired 3-D seismic data that, for the first time, precisely imaged sub-Zechstein (i.e. sub-evaporitic) upper Palaeozoic successions in NW Poland in order to develop a quantitative, balanced 2-D model of the late Palaeozoic–recent evolution of this area, characterised by a complex pattern of repeated extension and inversion. Four main tectonic phases have been determined: (1) Late Devonian–early Carboniferous extension and subsidence possibly related to extensional reactivation of Caledonian thrusts, (2) late Carboniferous inversion caused by the Variscan orogeny, (3) Permo-Mesozoic subsidence related to the development of the Polish Basin and (4) its Late Cretaceous–Paleogene inversion. Variscan and Alpine structures form a superimposed multilayer inversion system, mechanically decoupled by the Zechstein evaporites.
ISSN:1869-9529
1869-9510
1869-9529
DOI:10.5194/se-13-639-2022