Contrasting Early Carboniferous field geotherms - evidence for accretion of a thickened orogenic root and subducted Saxothuringian crust (Central European Variscides)
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F05%3A00008111" target="_blank" >RIV/00216208:11310/05:00008111 - isvavai.cz</a>
Alternative codes found
RIV/00216208:11310/05:8111
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Contrasting Early Carboniferous field geotherms - evidence for accretion of a thickened orogenic root and subducted Saxothuringian crust (Central European Variscides)
Original language description
Tectonic evolution of the western margin of the Bohemian Massif
Czech name
Kontrastní spodnokarbonské terénní geotermy - důkaz pro akreci ztlušťelého orogenního kořene a subdukované saxothuringické kůry (středoevropské Variscidy)
Czech description
Tektonický vývoj západního okraje Českého masivu
Classification
Type
J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)
CEP classification
DC - Seismology, volcanology and Earth structure
OECD FORD branch
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Result continuities
Project
<a href="/en/project/GA205%2F00%2F1526" target="_blank" >GA205/00/1526: Mass transfer during metamorphic reactions and its importance for textural changes in high-grade rocks</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>Z - Vyzkumny zamer (s odkazem do CEZ)
Others
Publication year
2005
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of the Geological Society London
ISSN
0016-7649
e-ISSN
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Volume of the periodical
162
Issue of the periodical within the volume
3
Country of publishing house
GB - UNITED KINGDOM
Number of pages
8
Pages from-to
463-470
UT code for WoS article
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EID of the result in the Scopus database
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