Exoskopie eolických sedimentů na Moravě

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985831%3A_____%2F04%3A00103920" target="_blank" >RIV/67985831:_____/04:00103920 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Exoscopy of Moravian eolian sediments

Popis výsledku v původním jazyce

Loess and related eolian sediment samples from selected localities in southern and central Moravia were studied using exoscopy combined with the study of heavy minerals, toward determining the provenance of their source rocks. The loess sediments from selected localities were divided into four sub-groups based on the characteristics of their heavy mineral fractions. Material of the first sub-group was deflated solely from the weathering horizons of nearby magmatic or metamorphic rocks to the west. The material of the other loess sub-areas was predominantly deflated from sedimentary rocks to the west, southwest, and northwest of their present sites. The sediments with a predominant fine-grained fraction contain exceedingly minimum quartz grains lackingdistinctive transport evidence. Nonetheless, it has been possible to use other methods in determining their source rocks.

Název v anglickém jazyce

Exoscopy of Moravian eolian sediments

Popis výsledku anglicky

Loess and related eolian sediment samples from selected localities in southern and central Moravia were studied using exoscopy combined with the study of heavy minerals, toward determining the provenance of their source rocks. The loess sediments from selected localities were divided into four sub-groups based on the characteristics of their heavy mineral fractions. Material of the first sub-group was deflated solely from the weathering horizons of nearby magmatic or metamorphic rocks to the west. The material of the other loess sub-areas was predominantly deflated from sedimentary rocks to the west, southwest, and northwest of their present sites. The sediments with a predominant fine-grained fraction contain exceedingly minimum quartz grains lackingdistinctive transport evidence. Nonetheless, it has been possible to use other methods in determining their source rocks.

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

Z - Vyzkumny zamer (s odkazem do CEZ)

Rok uplatnění

2004

Kód důvěrnosti údajů

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

Název periodika

Bulletin of Geosciences

ISSN

1214-1119

e-ISSN

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Svazek periodika

79

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

6

Strana od-do

177-182

Kód UT WoS článku

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EID výsledku v databázi Scopus

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