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- W2524104594 abstract "In the area of northwestern Croatia springs of thermal waters are much more common than the mineral and thermomineral ones. In this area thermal waters have been explored for last twenty years by numerous boreholes, but In the paper are presented only those data which have been obtained through the projects carried out by the Geological Institute of Zagreb. The exploration was realized through the projects Geothermal map of the Republic of Croatia and Geological monographs on thermal and mineral springs of the Republic of Croatla. It was found out during the exploration that thermal water occurrences are related to certain lithostratigraphic and tectonic conditions which must be fullfilled that the waters spout out at the surface or to be accumulated In the underground. The most important factor Is the existence of deep folds containing water-bearing strata and the link of water-carriers with the areas of collection of atmospheric waters and with the zones where water-carriers reach near-surface areas. Underground circulation of waters depends strongly on the degree of crushing and karstification of carbonate rocks as a consequence of strong tectonic movements and long-lasting breaks In sedimentation, i.e., the erosion." @default.
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- W2524104594 date "1999-01-01" @default.
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- W2524104594 title "Geological aspects of thermal and mineral water occurrences of northwestern Croatia" @default.
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