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

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F14%3A00000149" target="_blank" >RIV/00025798:_____/14:00000149 - isvavai.cz</a>

Výsledek na webu

<a href="http://sp.lyellcollection.org/content/405/1/NP.full.pdf+html" target="_blank" >http://sp.lyellcollection.org/content/405/1/NP.full.pdf+html</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1144/SP405.15" target="_blank" >10.1144/SP405.15</a>

Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

This volume summarizes the state of the art of Variscan geology from Iberia to the Bohemian Massif. The European Variscan belt consists of two orogens: the older, northern and the younger, southern. The northern Variscan realm was dominated by Late Devonian ? Carboniferous rifting, subduction and collisional events as defined by sedimentary records, crustal growth, recycling of continental crust and large-scale defor- mations. In contrast, the southern European crust was reworked by major Late Carboniferous collision fol- lowed by Permian wrenching. The Late Carboniferous ? Permian orogeny overprinted the previously accreted system in the north, but with much lower intensity, resulting in magmatic recycling and extensional tectonics. These two main orogenic cycles do not reflect episodic evolution of a single orogenic system but a complete change in orientation of stress field, thermal regime, degree of reworking and recycling of European crust, reflecting a major switch in plate confi

Název v anglickém jazyce

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

Popis výsledku anglicky

This volume summarizes the state of the art of Variscan geology from Iberia to the Bohemian Massif. The European Variscan belt consists of two orogens: the older, northern and the younger, southern. The northern Variscan realm was dominated by Late Devonian ? Carboniferous rifting, subduction and collisional events as defined by sedimentary records, crustal growth, recycling of continental crust and large-scale defor- mations. In contrast, the southern European crust was reworked by major Late Carboniferous collision fol- lowed by Permian wrenching. The Late Carboniferous ? Permian orogeny overprinted the previously accreted system in the north, but with much lower intensity, resulting in magmatic recycling and extensional tectonics. These two main orogenic cycles do not reflect episodic evolution of a single orogenic system but a complete change in orientation of stress field, thermal regime, degree of reworking and recycling of European crust, reflecting a major switch in plate confi

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 frmation of the European crust

ISBN

978-1-86239-658-6

Počet stran výsledku

7

Strana od-do

1-6

Počet stran knihy

406

Název nakladatele

The Geological Society of London

Místo vydání

London

Kód UT WoS kapitoly

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