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
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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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
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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