Zoisite-rich rock as a result of gabbro metasomatism, Újezd u Kunštátu, Letovice Complex
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F13%3A00000223" target="_blank" >RIV/00025798:_____/13:00000223 - isvavai.cz</a>
Result on the web
<a href="http://www.geology.cz/zpravy/obsah/2012/Zpravy_2012-50.pdf" target="_blank" >http://www.geology.cz/zpravy/obsah/2012/Zpravy_2012-50.pdf</a>
DOI - Digital Object Identifier
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Alternative languages
Result language
čeština
Original language name
Zoisitovec jako výsledek metasomatické přeměny metagabra, Újezd u Kunštátu, letovické krystalinikum
Original language description
A zoisite-rich rock associated mainly with ultabasic rocks occurs NE of Kunštát in the Letovice Complex. The zoisite-rich rock shows textures and geochemical features typical for metagabbros. Mineralogical composition and geochemical signature related toits cumulate origin was subsequently modified by extensive hydrothermal activites. The pre-Variscan metasomatic processes led to complete replacement of primary magmatic grains of calcic plagioclase by zoisite. The following Variscan stages of evolutionof the continental crust resulted in amphibolite facies metamorphism and incorporation of originally oceanic crust into the current position
Czech name
Zoisitovec jako výsledek metasomatické přeměny metagabra, Újezd u Kunštátu, letovické krystalinikum
Czech description
A zoisite-rich rock associated mainly with ultabasic rocks occurs NE of Kunštát in the Letovice Complex. The zoisite-rich rock shows textures and geochemical features typical for metagabbros. Mineralogical composition and geochemical signature related toits cumulate origin was subsequently modified by extensive hydrothermal activites. The pre-Variscan metasomatic processes led to complete replacement of primary magmatic grains of calcic plagioclase by zoisite. The following Variscan stages of evolutionof the continental crust resulted in amphibolite facies metamorphism and incorporation of originally oceanic crust into the current position
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
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2013
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Zprávy o geologických výzkumech v roce 2012
ISSN
0514-8057
e-ISSN
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Volume of the periodical
Neuveden
Issue of the periodical within the volume
podzim
Country of publishing house
CZ - CZECH REPUBLIC
Number of pages
4
Pages from-to
249-252
UT code for WoS article
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EID of the result in the Scopus database
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