Pregled bibliografske jedinice broj: 15914
A basis for the evaluation of geotechnical hazard of the Medvednica submountain area under dynamic conditions
A basis for the evaluation of geotechnical hazard of the Medvednica submountain area under dynamic conditions // Geotechnical hazards, Proceedings / Marić, Božica ; Lisac, Zvonimir ; Szavits - Nossan, Antun (ur.).
Rotterdam : Boston (MA) : Taipei: A.A. Balkema Publishers, 1998. str. 827-834 (predavanje, domaća recenzija, cjeloviti rad (in extenso), znanstveni)
CROSBI ID: 15914 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
A basis for the evaluation of geotechnical hazard of the Medvednica submountain area under dynamic conditions
Autori
Jurak, Vladimir ; Matković, Ivan ; Miklin Željko ; Cvijanović, Dragutin
Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni
Izvornik
Geotechnical hazards, Proceedings
/ Marić, Božica ; Lisac, Zvonimir ; Szavits - Nossan, Antun - Rotterdam : Boston (MA) : Taipei : A.A. Balkema Publishers, 1998, 827-834
Skup
XI th Danube - European conference on soil mechanics and geotehnical engineering
Mjesto i datum
Poreč, Hrvatska, 25.05.1998. - 29.05.1998
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Domaća recenzija
Ključne riječi
landslides; unstable slopes; earthquakes; triggering factor
Sažetak
In the Zagreb wider area the Medvednica submountain area is considered as a separate geotechnical macro-zone distinguished by a considerable density of unstable slopes and landslides. The mentioned zone is a densely constructed residential area.The respective zone is affected by the known hypocentre in the Medvednica massif in which the earthquakes with a magnitude M > 5,5 may be expected. In the last hundred years there were three earthquakes generated in the mentioned massif. The expected response of the slope to the seismic excitation defined by the adopted dynamic parameters can be reflected in two ways:
-either as a total failure of the slope previously affected by slow sliding;-or as initial deformations of the slope.
Both of these two ways open the access for other factors, meteorological and anthropogenic in particular. The gradation of these results is likely to point out to the necessity of slope zoning after the degree of stability and the relating slide risk.
Izvorni jezik
Engleski
Znanstvena područja
Geologija