New approach to garnet redistribution during aeolian transport
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F09%3A00334682" target="_blank" >RIV/67985831:_____/09:00334682 - isvavai.cz</a>
Alternative codes found
RIV/00025798:_____/09:00000529
Result on the web
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DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
New approach to garnet redistribution during aeolian transport
Original language description
Garnet composit ion within Late Pleistocene (Wechselian) loess and loess-like deposits was studied in 13 samples of sediment heavy mineral fractions from Moravia and Silesia (Czech Republic). Four areas differing in garnet geochemistry were identified and some regional trends in garnet composition changes were documented. The data obtained support the generally accepted conclusion of prevailing westerly winds during Weichselian loess deposition. Metamorphic rocks of the Bohemian Massif together with contributions from igneous (mainly granitic) and sedimentary rocks were indicated as a sourse for the Weichselian loess and loess-like deposits studied. Local differences in garnet composition depend on the basement source rocks, on prevailing wind direction, on regional geomoprphology and on transport distance.
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
Z - Vyzkumny zamer (s odkazem do CEZ)
Others
Publication year
2009
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Geological Quarterly
ISSN
1641-7291
e-ISSN
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Volume of the periodical
53
Issue of the periodical within the volume
3
Country of publishing house
PL - POLAND
Number of pages
8
Pages from-to
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UT code for WoS article
000271379700006
EID of the result in the Scopus database
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