Based on the first appearance datum of Hindeodus parvus in the section of the Žiri area it was possible to define paleontologically the Permian-Triassic boundary in Slovenia for the first time. Based on the conodont taxa H. parvus, Hindeodus typicalis, Hindeodus sp., Isarcicella isarcica, Isarcicella lobata, Isarcicella staeschei, Isarcicella turgida, and Isarcicella sp. At least three faunas can be distinguished, and they make possible a worldwide correlation. In a frame of this program we expanded our studies also to wider area of Dinarides (Aljinović et al. 2006, Sudar et al. 2007).
COBISS.SI-ID: 1427797
For the purpose of landslide susceptibility assessment the study area in the central Slovenia was divided to 78 365 slope units, for which 24 statistical variables were calculated Using multivariate statistical analysis (factor analysis), the interactions between factors and landslide distribution were tested, and the importance of individual factors for landslide occurrence was defined. Using probability measures, potentially hazardous areas were located in relation to population and road distribution, and hazard classes were assessed.
COBISS.SI-ID: 1202005
In the Bovec basin, which has been struck by 1998 and 2004 earthquakes, the resonance effects were studied by 124 free-field measurements in an area of 7 km2 and by measurements inside 20 buildings. The frequency range of increased vulnerability for buildings which prevail is 7-11 Hz. This range overlaps with fundamental frequency range of 6-12 Hz, which prevails in the map of free-field measurements. This indicates that the danger of soil-structure resonance is considerable in the area and has enhanced the damage to buildings. Variable sed. sequence in the basin contributes to variability.
COBISS.SI-ID: 1398613
This paper sets out to investigate which simple rotational body best fits the geometry of 38 dolines studied within the Classical Karst of Slovenia. It transpires that doline radius to depth ratio changes as a function of volume, whereas the mode of change remains stable regardless of the actual dimensions of individual dolines, and is basically the same at different locations. Doline volumes are very close of those of regular cones of the same dimensions, growing relatively deeper as the volume increases. Two poly-segment models implied by the power function model are discussed.
COBISS.SI-ID: 554334
We are specifically pointing out activities of the research group in the field of elaboration of new geological maps. By the end of the program period and/or in 2009, five new geological maps were/will be published. All were elaborated by researchers that either belong to the research group or are acting within its organizational framework.
COBISS.SI-ID: 238635776