Formation of a Composite Albian–Eocene Orogenic Wedge in the Inner Western Carpathians: P–T Estimates and 40Ar/39Ar Geochronology from Structural Units

Autor: Alexandra Molnárová, Ondrej Nemec, Ján Soták, Fred Jourdan, Čestmír Tomek, Marián Putiš, Peter Ružička, Martin Danišík

Publikováno v: Minerals
Volume 11
Issue 9
Minerals, Vol 11, Iss 988, p 988 (2021)

The composite Albian–Eocene orogenic wedge of the northern part of the Inner Western Carpathians (IWC) comprises the European Variscan basement with the Upper Carboniferous–Triassic cover and the Jurassic to Upper Cretaceous sedimentary successio

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9418d1ab0ded139d3603dc9368b0c0fd

Carpathian Shear Corridor – A strike-slip boundary of an extruded crustal segment

Autor: Paul Andriessen, Lucia Fojtíková, Vladimír Bezák, Marián Bošanský, Čestmír Tomek, František Marko, Milan Piovarči, Peter Reichwalder

Publikováno v: Marko, F, Andriessen, P A M, Tomek, Č, Bezák, V, Fojtíková, L, Bošanský, M, Piovarči, M & Reichwalder, P 2017, ' Carpathian Shear Corridor – A strike-slip boundary of an extruded crustal segment ', Tectonophysics, vol. 703-704, pp. 119-134 . https://doi.org/10.1016/j.tecto.2017.02.010
Tectonophysics, 703-704, 119-134. Elsevier

The Carpathian Shear Corridor (CSC), a morphostructurally distinctive ENE-WSW brittle shear zone, is a prominent dynamic interface of crustal fragments shifted during an oblique collision process combined with lateral extrusions in the Late stages of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c3467250d530efcc08e985041973ec92
https://doi.org/10.1016/j.tecto.2017.02.010

Petrogenesis of Miocene alkaline volcanic suites from western Bohemia: whole rock geochemistry and Sr–Nd–Pb isotopic signatures

Autor: Kadosa Balogh, Jaromír Ulrych, Anna Ladenberger, Čestmír Tomek, Lukáš Krmíček, Lukáš Ackerman, Felicity E. Lloyd

Publikováno v: Geochemistry. 76:77-93

The Mid to Late Miocene intraplate alkaline volcanic suites of western Bohemia are relict of the intensive voluminous volcanism accompanied by large-scale uplift and doming. The association with the uplift of the NE flank of the Cheb–Domažlice Gra

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::53b3c2c5b01bcf4c68bf2d3dffef9abd
https://doi.org/10.1016/j.chemer.2015.11.003

Structure of unmetamorphosed Variscan tectonic units of the southern Moravo-Silesian zone, Bohemian Massif: a review

Autor: Rostislav Melichar, Čestmír Tomek, Jiří Otava, Ondřej Bábek, Jiří Kalvoda

Publikováno v: Scopus-Elsevier

The Moravo-Silesian zone is a zone with alpine-type tectonics with typical juxtaposition of nappe units defined by diferrent devonian facies.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cba091981bb6bea14e29d75d20400f60
https://doi.org/10.1127/njgpa/239/2006/37

Large-scale thin-skinned tectonics in the eastern boundary of the Bohemian Massif

Autor: Čestmír Tomek, Pavel Cizek

Publikováno v: Tectonics. 10:273-286

Two new seismic reflection profiles and a deep borehole reveal thin-skinned thrusting on the easternmost part of the Rheno-Hercynian zone of the Variscan belt of Europe. Above Precambrian Brunnia basement the profiles show three different seismic zon

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5e207505aa4054b14142a088c5e10979
https://doi.org/10.1029/89tc03241