Trace elements in quartz from Li-enriched pegmatite

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F14%3A00434564" target="_blank" >RIV/67985831:_____/14:00434564 - 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

Trace elements in quartz from Li-enriched pegmatite

Original language description

Quartz from complex LCT pegmatites has similar evolutionary trend as quartz from fractionated granites: systematic increase of Al, Li, and Ge. In comparison with the most fractionated peraluminous granites, pegmatitic quartz is relatively depleted in Li,but strongly enriched in Ge. Minerals associated with crystallizing quartz may strongly influence the distribution of trace elements between quartz and melt. This influence is stronger in the pegmatitic than granitic melt.

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

DB - Geology and mineralogy

OECD FORD branch

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Project

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Continuities

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year

2014

Confidentiality

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

Name of the periodical

Mitteilungen der Österreichischen Mineralogischen Gesellschaft

ISSN

1609-0144

e-ISSN

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Volume of the periodical

160

Issue of the periodical within the volume

1

Country of publishing house

AT - AUSTRIA

Number of pages

6

Pages from-to

31-36

UT code for WoS article

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EID of the result in the Scopus database

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