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

Kód výsledku v 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>

Výsledek na webu

<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>

Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

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

Popis výsledku anglicky

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.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

<a href="/cs/project/GX19-27682X" target="_blank" >GX19-27682X: Hlavní mechanismy periferálního kontinentálního růstu během superkontinentálního cyklu</a><br>

Návaznosti

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

Rok uplatnění

2021

Kód důvěrnosti údajů

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

Název periodika

Earth-Science Reviews

ISSN

0012-8252

e-ISSN

—

Svazek periodika

220

Číslo periodika v rámci svazku

September : 103700

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

65

Strana od-do

nestránkováno

Kód UT WoS článku

000709289100002

EID výsledku v databázi Scopus

2-s2.0-85109463033