Brus Landslide, translational block sliding in flysch rock mass (CROSBI ID 559650)
Prilog sa skupa u zborniku | izvorni znanstveni rad | međunarodna recenzija
Podaci o odgovornosti
Arbanas, Željko ; Mihalić, Snježana ; Grošić, Mirko ; Dugonjić, Sanja ; Vivoda, Martina
engleski
Brus Landslide, translational block sliding in flysch rock mass
The Brus Landslide occurred in April 2005, near village Brus in Istria, Croatia. The Landslide is a typical translational block slide and the landslide body consists of practically unique flysch rock mass block, 150 m long and 35 m wide. Sliding occurred abruptly, without previous announcement signs of possible instability. The area of North Istria is composed of flysch deposits of Paleogene age. Superficial deposits are made of considerable thick packages, with alternating layers of siltstones, marls and sandstones. Landslide body is composed of flysch rock mass which is 10 m thick. Sliding surface is formed through bedding planes of siltstone layers. The sliding was caused by the unfavorable dip orientation of deposit layers in the slope, and additionally by the river erosion in the toe in combination with unfavorable hydrogeological conditions.
Brus landslide; translational block slide; flysch rock mass
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
Podaci o prilogu
635-638.
2010.
objavljeno
Podaci o matičnoj publikaciji
Rock Mechanics in Civil and Environmental Engineering. Proceedings of the European Rock Mechanics Symposium (Eurock 2010)
Zhao, Jian ; Labiouse, Vincent ; Dudt, Jean-Paul ; Mathier, Jean-Francois
London : Delhi: CRC Press ; A.A. Balkema Publishers
978-0-415-58654-2
Podaci o skupu
European Rock Mechanics Symposium (Eurock 2010)
predavanje
15.06.2010-18.06.2010
Lausanne, Švicarska