Devonian?Permian magmatic pulses in the northern Vosges Mountains (NE France): result of continuous subduction of the Rhenohercynian Ocean and Avalonian passive margin
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F14%3A00000095" target="_blank" >RIV/00025798:_____/14:00000095 - isvavai.cz</a>
Result on the web
<a href="http://sp.lyellcollection.org/content/405/1/197.abstract" target="_blank" >http://sp.lyellcollection.org/content/405/1/197.abstract</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1144/SP405.12" target="_blank" >10.1144/SP405.12</a>
Alternative languages
Result language
angličtina
Original language name
Devonian?Permian magmatic pulses in the northern Vosges Mountains (NE France): result of continuous subduction of the Rhenohercynian Ocean and Avalonian passive margin
Original language description
Middle Devonian?Permian magmatic rocks from the northern Vosges Mountains show temporal and chemical variations which are linked to the continuous subduction of the Rhenohercynian oceanic crust and the Avalonian Devonian passive margin underneath the Saxothuringian continental crust. Major and trace elements and Sr?Nd isotopes of the northern Vosges basic to acidic magmatic rocks show that they evolved through time from: (1) Middle Devonian tholeiitic to calc-alkaline volcanic Rabodeau?Schirmeck sequence derived from partial melting of a depleted mantle, with these primary magmas having triggered anatexis of young crustal material of the Saxothuringian crust; (2) calc-alkaline Bande Médiane volcanic belt (c. 334 Ma), diorite and Hohwald granodiorite intrusion (c. 329 Ma) originated from enriched mantle contaminated and metasomatized by fluids expelled from a subduction zone; (3) high-K calc-alkaline Belmont granite (c. 318 Ma), whose chemical signature suggests magma-mixing between enr
Czech name
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Czech description
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Classification
Type
C - Chapter in a specialist book
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
<a href="/en/project/LK11202" target="_blank" >LK11202: The role of Paleozoic accretionary and collisanal orogens on the formation and growth of continental crust</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2014
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Book/collection name
The Variscan orogeny: extent, timescale and the formation of the European crust
ISBN
978-1-86239-658-6
Number of pages of the result
26
Pages from-to
197-223
Number of pages of the book
406
Publisher name
The Geological Society of London
Place of publication
London
UT code for WoS chapter
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