K-rich magmatism in the Moldanubian Unit, Bohemian Massif ? a complex story featuring variably enriched lithospheric mantle melts and their interaction with the crust

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F03%3A00000147" target="_blank" >RIV/00025798:_____/03:00000147 - isvavai.cz</a>

Result on the web

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DOI - Digital Object Identifier

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Result language

angličtina

Original language name

K-rich magmatism in the Moldanubian Unit, Bohemian Massif ? a complex story featuring variably enriched lithospheric mantle melts and their interaction with the crust

Original language description

Primitive chemistry of the mafic rocks (highCr,Ni,mg#) argues for derivation from enriched mantle (Sr/Sri>0.712,Epsi~-7.5). Correlations of Sr-Nd isotopes with other parameters require genesis of K-rich plutonic rocks by mixing of 2 distinct magmas.

Czech name

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Czech description

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Type

J_x - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

CEP classification

DD - Geochemistry

OECD FORD branch

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Project

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Continuities

Z - Vyzkumny zamer (s odkazem do CEZ)

Publication year

2003

Confidentiality

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Name of the periodical

Geolines

ISSN

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e-ISSN

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Volume of the periodical

16

Issue of the periodical within the volume

duben

Country of publishing house

CZ - CZECH REPUBLIC

Number of pages

2

Pages from-to

48-49

UT code for WoS article

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EID of the result in the Scopus database

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