The Moldanubian Zone in the French Massif Central, Vosges/Schwarzwald and Bohemian Massif revisited: differences and similarities

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F14%3A00000093" target="_blank" >RIV/00025798:_____/14:00000093 - isvavai.cz</a>

Výsledek na webu

<a href="http://sp.lyellcollection.org/content/405/1/7.abstract" target="_blank" >http://sp.lyellcollection.org/content/405/1/7.abstract</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1144/SP405.14" target="_blank" >10.1144/SP405.14</a>

Jazyk výsledku

angličtina

Název v původním jazyce

The Moldanubian Zone in the French Massif Central, Vosges/Schwarzwald and Bohemian Massif revisited: differences and similarities

Popis výsledku v původním jazyce

In order to portray the main differences and similarities between the Northeastern Variscan segments (French Massif Central (FMC), Vosges, Black Forest and Bohemian Massif (BM)), we review their crustal-scale architectures, the specific rock associationsand lithotectonic sequences, as well as the ages of the main magmatic and metamorphic events. This review demonstrates significant differences between the 'Moldanubian? domains in the BM and the FMC. On this basis we propose distinguishing between the Eastern and Western Moldanubian zones, while the Vosges/Black Forest Mountains are an intermediate section between the BM and the FMC. The observed differences are the result of, first, the presence in the French segment of an early large-scale accretionary system prior to the main Variscan collision and, second, the duration of Saxothuringian/Armorican subduction, which generated long-lived magmatic arc and back-arc systems in the Bohemian segment, while the magmatic activity in the FMC

Název v anglickém jazyce

The Moldanubian Zone in the French Massif Central, Vosges/Schwarzwald and Bohemian Massif revisited: differences and similarities

Popis výsledku anglicky

In order to portray the main differences and similarities between the Northeastern Variscan segments (French Massif Central (FMC), Vosges, Black Forest and Bohemian Massif (BM)), we review their crustal-scale architectures, the specific rock associationsand lithotectonic sequences, as well as the ages of the main magmatic and metamorphic events. This review demonstrates significant differences between the 'Moldanubian? domains in the BM and the FMC. On this basis we propose distinguishing between the Eastern and Western Moldanubian zones, while the Vosges/Black Forest Mountains are an intermediate section between the BM and the FMC. The observed differences are the result of, first, the presence in the French segment of an early large-scale accretionary system prior to the main Variscan collision and, second, the duration of Saxothuringian/Armorican subduction, which generated long-lived magmatic arc and back-arc systems in the Bohemian segment, while the magmatic activity in the FMC

Druh

C - Kapitola v odborné knize

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

<a href="/cs/project/LK11202" target="_blank" >LK11202: Role paleozoických akrečních a kolizních orogénů na tvorbu a růst kontinentální kůry</a><br>

Návaznosti

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

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název knihy nebo sborníku

The Variscan orogeny: extent, timescale and the formation of the European crust

ISBN

978-1-86239-658-6

Počet stran výsledku

37

Strana od-do

7-44

Počet stran knihy

406

Název nakladatele

The Geological Society of London

Místo vydání

London

Kód UT WoS kapitoly

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