Trace elements in garnets of felsic granulites as sediment provenance indicators.

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F03%3A00000079" target="_blank" >RIV/00025798:_____/03:00000079 - isvavai.cz</a>

Alternative codes found

RIV/00216224:14310/03:00058723

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 garnets of felsic granulites as sediment provenance indicators.

Original language description

The Lower Carboniferous Culm Basin is part of the larger European Variscan foreland basin. The youngest sediments of the Myslejovice Formation contain heavy mineral assemblages dominated by pyrope-almandine garnets. This paper compares the major element(electron microprobe) and trace element (LA-ICP-MS) compositions of detrital pyrope-almandine garnets from the Luleč Conglomerates with garnets from granulites of the Czech Massif for the purpose of provenance study. At the present-day level of erosion fthe Bohemian Massif, granulite garnets have higher calcium and/or lower magnesium concentrations. The compositions and zoning patterns of pyrope-almandine garnets from the Luleč quarry compare well with granulite garnets from the Miroslav Crystalline

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

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

Journal of the Czech Geological Society

ISSN

1210-8197

e-ISSN

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Volume of the periodical

48

Issue of the periodical within the volume

02/01/04

Country of publishing house

CZ - CZECH REPUBLIC

Number of pages

2

Pages from-to

34-35

UT code for WoS article

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EID of the result in the Scopus database

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