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Record type:	stať ve sborníku (D)
Home Department:	Katedra fyzické geografie a geoekologie (31600)
Title:	Low-gradient megalandslides at the northern boundary of the Caucasus-Crimean orogene: seismically induced?
Citace	Pánek, T., Hradecký, J., Šilhán, K., Strom, A., Smolková, V. a Zerkal, O. Low-gradient megalandslides at the northern boundary of the Caucasus-Crimean orogene: seismically induced?. In: Earthquake-Induced Landslides, Proceedings of the International Symposium on Earthquake-Induced Landslides. Heidelberg: Springer, 2013. Springer, 2013. s. 243-252. ISBN 978-3-642-32237-2.

Subtitle
Publication year:	2013
Obor:	Zemský magnetismus, geodesie, geografie
Number of pages:	10
Page from:	243
Page to:	252
Form of publication:	Tištená verze
ISBN code:	978-3-642-32237-2
ISSN code:
Proceedings title:	Earthquake-Induced Landslides, Proceedings of the International Symposium on Earthquake-Induced Landslides
Proceedings:	Mezinárodní
Publisher name:	Springer
Place of publishing:	Heidelberg
Country of Publication:	Sborník vydaný v zahraničí
Název konference:	Earthquake-Induced Landslides
Místo konání konference:	Kiryu, Japan
Datum zahájení konference:
Typ akce podle státní příslušnosti účastníků:	Celosvětová akce
WoS code:
EID:

Key words in English:	Megalandslide dating;clay-rich substratum; Caucasus-Crimean thrust-and fold belt.
Annotation in original language:	We have detected at least 16 extremely large landslides (0.2 - 2.8 km3) in an ~ 800 km long stretch of the hilly northern foothills of the Caucasus-Crimean orogene (Russia, Ukraine). All landslides originated within tectonically inverted foredeep basins formed predominantly by the Neogene clay-rich substratum (claystones, marls and occasionally limestones). The landslides, which evolved as blockslides combined in their distal parts with earthflows, are characterized by an extremely low height to length ratio (0.05-0.08). OSL and radiocarbon dating of deposits of the selected landslides pointed to various stages of the Last Glacial and Holocene.
Annotation in english language:

References

Reference

R01:	RIV/61988987:17310/13:A13017F7

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