Controls on Development of Asymmetric Fining-Upward Megacycles in a Generally fine-Grained Turbidite System of the Moravice Formation, Moravian-Silesian Culm Basin

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989592%3A15310%2F01%3A00001186" target="_blank" >RIV/61989592:15310/01:00001186 - isvavai.cz</a>
Alternative codes found
RIV/67985831:_____/01:09013086
Result on the web
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DOI - Digital Object Identifier
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Result language
angličtina
Original language name
Controls on Development of Asymmetric Fining-Upward Megacycles in a Generally fine-Grained Turbidite System of the Moravice Formation, Moravian-Silesian Culm Basin
Original language description
The Moravian-Silesian Culm basin filled with varied, mainly deep-marine siliciclastic sediments has undergone a large-scale syn-and postsedimenary tectonic evolution in a ocean subduction (remnant basin) to continental collision (foreland basin) relatedtectonic setting (Kumpera and Martinec 1995), leading to its complexity in the present-day tectonic structure and facies architecture.
Czech name
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Czech description
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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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Project
<a href="/en/project/GA205%2F00%2F0118" target="_blank" >GA205/00/0118: Facies architecture of the turbidite system of Moravice formation, Nízký Jeseník culm basin, based on sedimentology and ichnofacies analysis</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2001
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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