Paleogeographical and Paleo-Geodynamic Context of the Variscan Belt

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F23%3A10168738" target="_blank" >RIV/00025798:_____/23:10168738 - isvavai.cz</a>

Výsledek na webu

<a href="https://doi.org/10.1002/9781394228966.ch2" target="_blank" >https://doi.org/10.1002/9781394228966.ch2</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1002/9781394228966.ch2" target="_blank" >10.1002/9781394228966.ch2</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Paleogeographical and Paleo-Geodynamic Context of the Variscan Belt

Popis výsledku v původním jazyce

Providing the paleogeographical and paleo-geodynamic context of the Variscan belt involves identifying the Paleozoic lithospheric plates, that is, the principal ?contributors? involved in forming this orogen and restoring the paleopositions of continents and oceans during this geological period. Strictly speaking, the only method to restore the paleopositions of continents is paleomagnetism. From a paleo-geodynamic point of view, litho-tectonic zonation on the scale of the European Variscan belt must also account for the occurrence in the Bohemian Massif, the Black Forest, Vosges, as in the French Massif Central, of magmatic arc systems. Major advances in terms of the precision of paleogeographic reconstructions were obtained by comparing all paleontological, paleo-climatological and mineralogical constraints with paleomagnetic data. Fossil magnetic field recording is indeed the most rigorous method for reproducing the movements and rotations of large continental domains.

Název v anglickém jazyce

Paleogeographical and Paleo-Geodynamic Context of the Variscan Belt

Popis výsledku anglicky

Providing the paleogeographical and paleo-geodynamic context of the Variscan belt involves identifying the Paleozoic lithospheric plates, that is, the principal ?contributors? involved in forming this orogen and restoring the paleopositions of continents and oceans during this geological period. Strictly speaking, the only method to restore the paleopositions of continents is paleomagnetism. From a paleo-geodynamic point of view, litho-tectonic zonation on the scale of the European Variscan belt must also account for the occurrence in the Bohemian Massif, the Black Forest, Vosges, as in the French Massif Central, of magmatic arc systems. Major advances in terms of the precision of paleogeographic reconstructions were obtained by comparing all paleontological, paleo-climatological and mineralogical constraints with paleomagnetic data. Fossil magnetic field recording is indeed the most rigorous method for reproducing the movements and rotations of large continental domains.

Druh

C - Kapitola v odborné knize

CEP obor

—

OECD FORD obor

10505 - Geology

Projekt

—

Návaznosti

V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Rok uplatnění

2023

Kód důvěrnosti údajů

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

Název knihy nebo sborníku

The Variscan Belt of Western Europe 1: History, Geodynamic Context and Early Orogenic Events

ISBN

978-1-78945-099-6

Počet stran výsledku

63

Strana od-do

47-109

Počet stran knihy

230

Název nakladatele

Wiley - ISTE

Místo vydání

Londýn

Kód UT WoS kapitoly

—