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Brus Landslide, translational block sliding in flysch rock mass


Arbanas, Željko; Mihalić, Snježana; Grošić, Mirko; Dugonjić, Sanja; Vivoda, Martina
Brus Landslide, translational block sliding in flysch rock mass // 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 (ur.).
London: CRC Press/Balkema, 2010. str. 635-638 (predavanje, međunarodna recenzija, cjeloviti rad (in extenso), znanstveni)


Naslov
Brus Landslide, translational block sliding in flysch rock mass

Autori
Arbanas, Željko ; Mihalić, Snježana ; Grošić, Mirko ; Dugonjić, Sanja ; Vivoda, Martina

Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni

Izvornik
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 : CRC Press/Balkema, 2010, 635-638

ISBN
978-0-415-58654-2

Skup
European Rock Mechanics Symposium (Eurock 2010)

Mjesto i datum
Laussane, Švicarska, 15-18.06.2010

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
Brus landslide; translational block slide; flysch rock mass

Sažetak
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.

Izvorni jezik
Engleski

Znanstvena područja
Građevinarstvo, Rudarstvo, nafta i geološko inženjerstvo



POVEZANOST RADA


Projekt / tema
082-0822161-2187 - Ispitivanje i modeliranje poboljšanog tla i stijene (Meho-Saša Kovačević, )
114-0822695-2568 - Procjena, umanjivanje i upravljanje geološkim hazardom u području Kvarnera (Čedomir Benac, )
195-1951825-1507 - Razvoj sustava upravljanja geotehničkim podacima za procjenu prirodnih hazarda (Predrag Kvasnička, )

Ustanove
Građevinski fakultet, Zagreb,
Građevinski fakultet, Rijeka,
Rudarsko-geološko-naftni fakultet, Zagreb