Evolution of the Czech part of the Smrčiny/Fichtelgebirge granite pluton.
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F01%3A08010025" target="_blank" >RIV/67985891:_____/01:08010025 - isvavai.cz</a>
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Evolution of the Czech part of the Smrčiny/Fichtelgebirge granite pluton.
Original language description
The Smrčiny/Fichtelgebirge pluton in the western part of the Bohemian massif is formed by various magmatic phases of biotite, two-mica and muscovite granites. The least evolved biotite granites G1 are transitional I/S granite with higher content of Ba, Th, Zr in comparison to their content in the continental crust and with higher ratio of LREE/HREE.
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
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Continuities
Z - Vyzkumny zamer (s odkazem do CEZ)
Others
Publication year
2001
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Acta Montana. series A - Geodynamics
ISSN
1211-1910
e-ISSN
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Volume of the periodical
N/A
Issue of the periodical within the volume
18(121)
Country of publishing house
CZ - CZECH REPUBLIC
Number of pages
9
Pages from-to
5-13
UT code for WoS article
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EID of the result in the Scopus database
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