Contrasting tectono-metamorphic evolution of orogenic lower crust in the Bohemian Massif: A numerical model
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F14%3A10133537" target="_blank" >RIV/00216208:11320/14:10133537 - isvavai.cz</a>
Alternative codes found
RIV/00216208:11310/14:10133537 RIV/00025798:_____/14:00000015
Result on the web
<a href="http://dx.doi.org/10.1016/j.gr.2012.08.020" target="_blank" >http://dx.doi.org/10.1016/j.gr.2012.08.020</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.gr.2012.08.020" target="_blank" >10.1016/j.gr.2012.08.020</a>
Alternative languages
Result language
angličtina
Original language name
Contrasting tectono-metamorphic evolution of orogenic lower crust in the Bohemian Massif: A numerical model
Original language description
The Bohemian Massif, located at the eastern margin of the European Variscan belt, is characterised by an exceptional accumulation of felsic high-pressure granulites. The petrological, structural and geochronological studies of this region revealed systematic differences between the tectonometamorphic evolution of the southern (Moldanubian) and northern (West Sudetes) parts of the orogen. Two contrasting tectonic scenarios have been proposed: gravity-driven vertical mass exchanges followed by continentalindentation in the Moldanubian domain, and crustal-scale folding leading to gneiss dome formation in the West Sudetes. We present a numerical model in order to correlate the apparent differences between these two regions with the variations in the dynamics of the modelled system. We model two colliding blocks: an orogenic root, where a felsic lower crust is overlain by a mafic layer and a middle crust, and a continental indentor. We examine the role of the rate of convergence of the two
Czech name
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Czech description
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Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DB - Geology and mineralogy
OECD FORD branch
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Result continuities
Project
Result was created during the realization of more than one project. More information in the Projects tab.
Continuities
S - Specificky vyzkum na vysokych skolach
Others
Publication year
2014
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Gondwana Research
ISSN
1342-937X
e-ISSN
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Volume of the periodical
25
Issue of the periodical within the volume
2
Country of publishing house
NL - THE KINGDOM OF THE NETHERLANDS
Number of pages
13
Pages from-to
509-521
UT code for WoS article
000333140600005
EID of the result in the Scopus database
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