Articles | Volume 13, issue 2
Solid Earth, 13, 393–416, 2022
https://doi.org/10.5194/se-13-393-2022
Solid Earth, 13, 393–416, 2022
https://doi.org/10.5194/se-13-393-2022
Research article
24 Feb 2022
Research article | 24 Feb 2022

Variscan structures and their control on latest to post-Variscan basin architecture: insights from the westernmost Bohemian Massif and southeastern Germany

Hamed Fazlikhani et al.

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Cited articles

Arthaud, F. and Matte, P.: Late Paleozoic strike-slip faulting in southern Europe and northern Africa: Result of a right-lateral shear zone between the Appalachians and the Urals, GSA Bulletin, 88, 1305–1320, https://doi.org/10.1130/0016-7606(1977)88<1305:LPSFIS>2.0.CO;2, 1977. 
Bader, K. and Bram, K. (Eds.): Der mittelfränkische Gebirgsrücken südlich Nürnberg: Geologischer Rahmen, geophysikalische Untersuchungen und Ergebnisse von Forschungsbohrungen, Geologisches Jahrbuch Reihe E, Band E 58, Schweizerbart and Borntraeger, Stuttgart, Germany, ISBN 978-3-510-95873-3, 2001. 
Ballèvre, M., Manzotti, P., and Dal Piaz, G. V.: Pre-Alpine (Variscan) Inheritance: A Key for the Location of the Future Valaisan Basin (Western Alps), Tectonics, 37, 786–817, https://doi.org/10.1002/2017TC004633, 2018. 
Behr, H. J. and Heinrichs, T.: Geological interpretation of DEKORP 2-S: A deep seismic reflection profile across the Saxothuringian and possible implications for the Late Variscan structural evolution of Central Europe, Tectonophysics, 142, 173–202, https://doi.org/10.1016/0040-1951(87)90122-3, 1987. 
Bergerat, F. and Geyssant, J.: Tectonique cassante et champ de contraintes tertiaire en avant des Alpes orientales: le Jura souabe, Geol. Rundsch., 71, 537–548, 1982. 
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Interpretation of newly acquired FRANKEN 2D seismic survey data in southeeastern Germany shows that upper Paleozoic low-grade metasedimentary rocks and possible nappe units are transported by Variscan shear zones to ca. 65 km west of the Franconian Fault System (FFS). We show that the locations of post-Variscan upper Carboniferous–Permian normal faults and associated graben and half-graben basins are controlled by the geometry of underlying Variscan shear zones.