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The Mid-Variscan Allochthon: Keys from correlation, partial retrodeformation and plate-tectonic reconstruction to unlock the geometry of a non-cylindrical belt

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F21%3A00000080" target="_blank" >RIV/00025798:_____/21:00000080 - isvavai.cz</a>

  • Result on the web

    <a href="https://www.sciencedirect.com/science/article/pii/S0012825221002014?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0012825221002014?via%3Dihub</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.earscirev.2021.103700" target="_blank" >10.1016/j.earscirev.2021.103700</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    The Mid-Variscan Allochthon: Keys from correlation, partial retrodeformation and plate-tectonic reconstruction to unlock the geometry of a non-cylindrical belt

  • Original language description

    The non-cylindrical character of the Variscan Belt is established via a description of its most salient geologicalcharacteristics and correlations among the main and relatively minor massifs from Bohemia to Morocco on thebasis of a bibliographical synthesis. Using the firmly established tectonostratigraphic domains, the continuity ofVariscan zones is discussed, as well as the western termination of the one that occupies most of the central part ofthe belt. This zone is characterized by its allochthony, and breaks the continuity of the zonation, that is, thecylindrism of the belt. A proposal is made to call this zone the Mid-Variscan Allochthon and its wedge shape inmap view is explained performing a step by step restoration of late Variscan deformation. Once the geometry ofthe belt is interpreted by a succession of regionally significant deformation events, a kinematic reconstruction isproposed. It is based on recent developments on the knowledge of Paleozoic plate tectonics and intended to showthat the deformation model is compatible with current paleogeographical developments.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10505 - Geology

Result continuities

  • Project

    <a href="/en/project/GX19-27682X" target="_blank" >GX19-27682X: Principal mechanisms of peripheral continental growth during supercontinent cycle</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2021

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Earth-Science Reviews

  • ISSN

    0012-8252

  • e-ISSN

  • Volume of the periodical

    220

  • Issue of the periodical within the volume

    September : 103700

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    65

  • Pages from-to

    nestránkováno

  • UT code for WoS article

    000709289100002

  • EID of the result in the Scopus database

    2-s2.0-85109463033