Palaeozoic evolution of the Variscan Vosges Mountains

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F14%3A00000094" target="_blank" >RIV/00025798:_____/14:00000094 - isvavai.cz</a>

Výsledek na webu

<a href="http://sp.lyellcollection.org/content/405/1/45.abstract" target="_blank" >http://sp.lyellcollection.org/content/405/1/45.abstract</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1144/SP405.8" target="_blank" >10.1144/SP405.8</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Palaeozoic evolution of the Variscan Vosges Mountains

Popis výsledku v původním jazyce

A geological synthesis of the Palaeozoic Vosges Mountains (NE France) is presented using existing observations and new data. The geodynamic evolution involves: (1) Early Palaeozoic sedimentation and magmatism; (2) Late Devonian subduction triggering back-arc spreading; (3) early Lower Carboniferous continental subduction, continent?continent collision and polyphase deformation and metamorphism of the orogenic root; and (4) late Lower Carboniferous orogenic collapse driven by thermal weakening of the middle crust. The evolution is integrated within the framework of the European Variscan Belt. The Northern Vosges comprise sediments of Rhenohercynian affinity separated from Teplá-Barrandian metasediments by a Lower Carboniferous magmatic arc. The latter is correlated with the Mid-German Crystalline Rise, and is ascribed to the south-directed subduction of the Rhenohercynian Basin. The Saxothuringian?Moldanubian suture is thought to be obliterated by the magmatic arc, while the Lalaye?Lubi

Název v anglickém jazyce

Palaeozoic evolution of the Variscan Vosges Mountains

Popis výsledku anglicky

A geological synthesis of the Palaeozoic Vosges Mountains (NE France) is presented using existing observations and new data. The geodynamic evolution involves: (1) Early Palaeozoic sedimentation and magmatism; (2) Late Devonian subduction triggering back-arc spreading; (3) early Lower Carboniferous continental subduction, continent?continent collision and polyphase deformation and metamorphism of the orogenic root; and (4) late Lower Carboniferous orogenic collapse driven by thermal weakening of the middle crust. The evolution is integrated within the framework of the European Variscan Belt. The Northern Vosges comprise sediments of Rhenohercynian affinity separated from Teplá-Barrandian metasediments by a Lower Carboniferous magmatic arc. The latter is correlated with the Mid-German Crystalline Rise, and is ascribed to the south-directed subduction of the Rhenohercynian Basin. The Saxothuringian?Moldanubian suture is thought to be obliterated by the magmatic arc, while the Lalaye?Lubi

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

30

Strana od-do

45-75

Počet stran knihy

406

Název nakladatele

Geological Society London

Místo vydání

London

Kód UT WoS kapitoly

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