Source composition and melting temperatures of the main granitic suites from the Moldanubian Batholith
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985891%3A_____%2F16%3A00470329" target="_blank" >RIV/67985891:_____/16:00470329 - isvavai.cz</a>
Result on the web
<a href="http://dx.doi.org/10.3190/jgeosci.223" target="_blank" >http://dx.doi.org/10.3190/jgeosci.223</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3190/jgeosci.223" target="_blank" >10.3190/jgeosci.223</a>
Alternative languages
Result language
angličtina
Original language name
Source composition and melting temperatures of the main granitic suites from the Moldanubian Batholith
Original language description
The granitoids of the Moldanubian Batholith are represented by three main suites: I- to I/S-type Weinsberg biotite granites–granodiorites, S-type Eisgarn two-mica granites and I/S-type Freistadt biotite granites–granodiorites. Partial melting of metapelites likely produced most of the Eisgarn suite at c. 775–825 ºC. Parental melts of the Weinsberg and Freistadt suites could have been generated by partial melting of a metagreywackes–metabasalts mixture at c. 740–940 ºC.
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
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2016
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 Geosciences
ISSN
1802-6222
e-ISSN
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Volume of the periodical
61
Issue of the periodical within the volume
4
Country of publishing house
CZ - CZECH REPUBLIC
Number of pages
16
Pages from-to
355-370
UT code for WoS article
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EID of the result in the Scopus database
2-s2.0-85011681623