The Slovenj Gradec Basin represents one of the marginal western basins of the Neogene Pannonian Basin system. Its sedimentary succession is investigated by combination of field, petrographic and ...geochemical methods. The succession is at least 540m thick and characterised by frequent alternation of conglomerate, sandstone, siltstone and marlstone deposited in terrestrial, brackish and shallow marine environments. Modal composition of the sandstones indicates that they originated from recycled orogen, namely from quartzose sedimentary rocks of the Eastern Alps, and show moderate to absent chemical weathering. The results indicate two different tectonic settings: a collisional, which correlates well with the end-Mesozoic and Cenozoic Alpine collision, resulting in orogeny and thrusting of the Austroalpine nappes, and a passive margin related to the early Neogene lithospheric extension and subsidence as the result of slab retreat in the Carpathian subduction zone, which was responsible for the formation of the Pannonian Basin system.
In this area, where the sediments were subjected to various tectonic events, discriminant function diagrams of Verma and Armstrong Altrin are found to be a good tool for their identification and differentiation.
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GEOZS, IJS, IMTLJ, KILJ, KISLJ, NLZOH, NUK, OILJ, PNG, SAZU, SBCE, SBJE, UL, UM, UPCLJ, UPUK, ZRSKP
The Miocene evolution of the area transitional from the Eastern Alps to the Pannonian Basin System was studied through the paleogeographic evolution of the Slovenj Gradec Basin in northern Slovenia. ...It is based on mapping, section logging, nannoplankton biostratigraphy, and petrography. The results are correlated with the lithological column of the borehole MD-1/05. The evolution of the basin is connected with the development of the Pannonian Basin System, and the global 3
order cycles, which influenced the connection with the Mediterranean Sea. Sedimentation started in the Karpatian in a fluvial to lacustrine environment and terminated at the end of the Early Badenian. During this period, three transgression–regression cycles were recorded. The first transgression occurred in the Karpatian and corresponds to the TB 2.2. cycle. The sediments reflect proximity of the hinterland. After a short break in sedimentation, the Early Badenian deposition followed. It marks the second transgression into the SGB, the first Badenian, correlated with the TB 2.3 cycle. There are signs of a transitional environment, which evolved to marine in advanced stages. At the high-stand system tract, the sea flooded the entire Slovenj Gradec Basin. Subsequent reduced quantity and diversity of the microfossils marks the onset of the second regression stage. It is followed by the third transgression, the second in the Badenian, correlated with the TB 2.4 cycle. The late Early Badenian deposition continued in the lower-energy, though occasionally still turbulent environment. Silty sediments with upward increasing content of organic matter indicate shallowing of the basin, until its final diminishing. Layers of fresh-water coal already bear witness to the existence of restricted swamps. After the Early Badenian, the area of the Slovenj Gradec Basin became dry land, exposed to erosion.
In Slovenia, mass movements are not only a threat to the population, but also a major environmental and social science challenge. Lithologically heterogeneous areas have been found to be problematic, ...and the Miocene Slovenj Gradec basin (in northeast Slovenia) is one such area. For this area, we developed landslide and rockfall susceptibility maps based on detailed geological research combined with statistical modeling schemes. Crucial factors include lithological composition, land use, geological structural elements, slope curvature, aspect and inclination, and bed dipping. The approach taken in the development of mass movement susceptibility maps presented here is transferable to other areas defined by heterogeneous lithology. Such maps could prove useful spatial planning, forestry, environmental protection, landscape architecture, and other fields.
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DOBA, IZUM, KILJ, NUK, PILJ, PNG, SAZU, UILJ, UKNU, UL, UM, UPUK
In the frame of national research and innovation project MASPREM exposure maps of inhabitants, buildings and infrastructures to landslide occurrence were developed for five selected Slovenian ...municipalities. Maps represent an upgrade of the landslide susceptibility maps that were elaborated based on synthesis of analysis of event-based landslide inventory and field investigations. Exposure maps were developed for five municipalities: Bovec, La{ko, Slovenj Gradec, Trbovlje and Železniki. Exposure of inhabitants, construction and infrastructures to landslide occurrence was analysed using simple cross-analysis of landslide susceptibility maps at scale of 1:25,000 with locations of exposed elements. All analyses were conducted in the GIS with software tool ArcMap. Exposure maps, based on landslide susceptibility, were classified into six classes, with values ranging from one to six where class one represents areas with negligible exposure and class six areas with very high exposure to landslide occurrence. Exposure maps of selected municipalities provide the basis for further assessment of risk and consequentially better risk management.
Članek obravnava navzočnost plemstva v srednjeveškem Slovenj Gradcu in v tem okviru tiste plemiške družine, ki so v mestu krajši ali daljši čas bivale v 14. in 15. stoletju. Kot drugod je tudi v ...Slovenj Gradcu predvsem plemstvo kmalu prepoznalo dobrodošel poligon za uresničevanje svojih gospodarskih, pa tudi političnih ambicij. Njegova navzočnost se v mestu začenja očitneje kazati v prvih desetletjih 14. stoletja, čeprav prva plemiška bivališča, t. i. stolpi, gotovo nastanejo že v prejšnjem stoletju. Najizrazitejši pečat vtisnejo Slovenj Gradcu med plemiči rodbini Muttlov in Trappov ter z Gorenjskega priseljeni Janez iz Loke, ustanovitelj meščanskega špitala. Le za člane družine Muttlov je sicer izpričano, da so opravljali meščanske funkcije in bili torej slovenjgraški meščani. Čeprav bi bilo v omenjenih plemičih pretirano videti zametke mestnega patriciata, so gotovo najodločilneje oblikovali mestno zgodovino v 14. in 15. stoletju.
Extended description:
Reportaža o transplantaciji kostnega mozga, panorama Slovenj Gradca, bolnišnica, govorijo, dr. Strnad - ravnatelj bolnišnice, dr. Ivo Rajšp - internist, Tone Britovšek - dajalec ...mozga.
Bolnišnica v Slovenj Gradcu je bila ustanovljena pred 70 leti, danes lahko nudi pomoč 228 bolnikom, že letos pa jo bodo povečali še za 170 postelj. Sicer pa, nas zanima predvsem presaditev kostnega mozga. Obiščimo najprej ravnatelja, primarija dr. Strnada in poslušajmo, kaj pravi on o tem pomembnem dogodku.
Izjava dr. Strnad.
Bodi karkoli, ti ljudje iz Slovenj Gradca so opravili veliko delo, upamo pa tudi, da bo njihovo prizadevanje rodilo, še bogate sadove, da bo njihovo delo še uspešnejše.
Information:
This is Slovenj Gradec, a town on the border between the Štajerska and Koroška regions. It is pleasant and homely, as with the majority of historical Slovene regional towns. Nevertheless, an important event has again drawn the attention of entire country recently. The Slovenj Gradec hospital was the venue of the first bone marrow transplant in Slovenia.
Original language summary:
To je Slovenj Gradec, mesto na meji med Štajersko in Koroško. Tako je, kot večina naših starih pokrajinskih mest; prijetno in domače. Toda pred nedavnim je pomemben dogodek spet ponesel ime tega mesta po vsej domovini. V slovenjgraški bolnišnici so prvič v Sloveniji presadili kostni mozeg.
The intention of the amendments and supplements to the spatial components of planning documents in the municipality of Slovenj Gradec are, amongst other, novelties to the master plans of particular ...settlements. The article presents motives and reasons for changing the master plan and the desired contents of a spatial document adapted to contemporary social and economic circumstances.
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