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

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About: The Moldanubian Zone in the French Massif Central, Vosges/Schwarzwald and Bohemian Massif revisited: differences and similarities Goto Sponge NotDistinct Permalink

An Entity of Type : http://linked.opendata.cz/ontology/domain/vavai/Vysledek, within Data Space : linked.opendata.cz associated with source document(s)

Attributes	Values
rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
rdfs:seeAlso	http://sp.lyellcollection.org/content/405/1/7.abstract
Description	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 associations and 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 was comparably short-lived. 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 associations and 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 was comparably short-lived. (en)
Title	The Moldanubian Zone in the French Massif Central, Vosges/Schwarzwald and Bohemian Massif revisited: differences and similarities The Moldanubian Zone in the French Massif Central, Vosges/Schwarzwald and Bohemian Massif revisited: differences and similarities (en)
skos:prefLabel	The Moldanubian Zone in the French Massif Central, Vosges/Schwarzwald and Bohemian Massif revisited: differences and similarities The Moldanubian Zone in the French Massif Central, Vosges/Schwarzwald and Bohemian Massif revisited: differences and similarities (en)
skos:notation	RIV/00025798:_____/14:00000093!RIV15-MSM-00025798
http://linked.open...avai/riv/aktivita	P
http://linked.open...avai/riv/aktivity	P(LK11202)
http://linked.open...vai/riv/dodaniDat	2015
http://linked.open...aciTvurceVysledku	Janoušek, Vojtěch Schulmann, Karel Lexa, Ondrej Štípská, Pavla
http://linked.open.../riv/druhVysledku	C - Kapitola v knize
http://linked.open...iv/duvernostUdaju	S - Úplné a pravdivé údaje nepodléhající ochraně podle zvláštních právních předpisů
http://linked.open...titaPredkladatele	Česká geologická služba
http://linked.open...dnocenehoVysledku	30261
http://linked.open...ai/riv/idVysledku	RIV/00025798:_____/14:00000093
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	Massif Central, Variscan (en)
http://linked.open.../riv/klicoveSlovo	Variscan Massif Central
http://linked.open...ontrolniKodProRIV	[FF86A977DE6C]
http://linked.open...i/riv/mistoVydani	London
http://linked.open...vEdiceCisloSvazku	Geological Society, London, Special Publications, 405
http://linked.open...i/riv/nazevZdroje	The Variscan orogeny: extent, timescale and the formation of the European crust
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	4 (xsd:int)
http://linked.open...v/pocetStranKnihy	406 (xsd:int)
http://linked.open...cetTvurcuVysledku	8 (xsd:int)
http://linked.open...vavai/riv/projekt	The role of Paleozoic accretionary and collisanal orogens on the formation and growth of continental crust
http://linked.open...UplatneniVysledku	2014
http://linked.open...iv/tvurceVysledku	Edel, Jean-Bernard Janoušek, Vojtěch Lexa, Ondrej Schulmann, Karel Štípská, Pavla Skrzypek, Etienne Faure, Michel Lardeaux, Jean-Marc
number of pages	37 (xsd:int)
http://bibframe.org/vocab/doi	10.1144/SP405.14
http://purl.org/ne...btex#hasPublisher	The Geological Society of London
https://schema.org/isbn	978-1-86239-658-6

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