Publ3 search

Error:

Javascript is disabled in this browser. This page requires Javascript. Modify your browser's settings to allow Javascript to execute. See your browser's documentation for specific instructions.

Publikační činnost

Probíhá načítání, čekejte prosím...

Typ záznamu * :	článek v odborném periodiku (J)
Domácí pracoviště * :	Katedra fyzické geografie a geoekologie (31600)
Název * :	Landslide complex in the northern part of the Silesian Beskydy Mountains (Czech Republic)
Citace :	Hradecký, J., Pánek, T. a Klimová, R. Landslide complex in the northern part of the Silesian Beskydy Mountains (Czech Republic). Landslides; Springer. 2007, č. 4, s. 53-62. ISSN 1612-510X.

Podnázev :
Rok * :	2007
Obor * :	Zemský magnetismus, geodesie, geografie
Kód ISSN * :	1612-510X
Oficiální název periodika * :	Landslides; Springer
Stát vydavatele periodika * :	Spolková republika Německo
Svazek periodika * :	4
Číslo periodika v rámci svazku * :	3
Číslo článku :
Ročník :
Počet stran článku * :	10
Strana od * :	53
Strana do * :	62
Kód UT WoS :	000244320300006
EID :
Poddruh recenzovaného článku :	Článek v impaktovaném časopise (Jimp)

Klíčová slova anglicky * :	Deep-seated gravitational slope deformations; Landslide complex; 14C dating; Geophysical sounding; Flysch; Silesian Beskydy Mountains; Czech Republic
Popis v původním jazyce * :	The study brings new information concerning a large slope deformation in the northern part of the Silesian Beskydy Mountains in the territory of the Czech Republic. The studied area is a large-scale transformation of the forefront of a flysch nappe formed especially by rigid sandstones upon a plastic underlying nappe. As a consequence of the vertical contact of mechanically different formations and depositing conditions of rocks and tectonics on the nappe forefront, several generations of deep-seated slope deformations occurred accompanied by shallow landslides in the historic period. Structural measurement and geophysical sounding proved prevailing lateral spreading in the upper parts of the slopes as well as the occurrence of rotational landslides whose landslide scarps overlap with the line of overthrust of the Godula Nappe on the Těšín Nappe. Radiocarbon dating determined the period of the occurrence of rotational landslides as falling into the Subboreal up to Subatlantic.
Popis v anglickém jazyce * :	The study brings new information concerning a large slope deformation in the northern part of the Silesian Beskydy Mountains in the territory of the Czech Republic. The studied area is a large-scale transformation of the forefront of a flysch nappe formed especially by rigid sandstones upon a plastic underlying nappe. As a consequence of the vertical contact of mechanically different formations and depositing conditions of rocks and tectonics on the nappe forefront, several generations of deep-seated slope deformations occurred accompanied by shallow landslides in the historic period. Structural measurement and geophysical sounding proved prevailing lateral spreading in the upper parts of the slopes as well as the occurrence of rotational landslides whose landslide scarps overlap with the line of overthrust of the Godula Nappe on the Těšín Nappe. Radiocarbon dating determined the period of the occurrence of rotational landslides as falling into the Subboreal up to Subatlantic.

Typ zdroje financování výsledku * :

Projekty CEP/Záměry CEZ

Seznam projektů :

ID Projektu	Název projektu

Seznam ohlasů :

Ohlas

R01:	RIV/61988987:17310/07:A0800H5Y

Complementary Content

${loading}