The Periadriatic lineament extends from the Sesia zone in Italyacross southern Austria into Slovenia, in the area of the Karavankemountains. It continues eastwards into the Pannonian basin in ...Hungaryas the Balaton line. The Karavanke mountain range runs fromSlovenia in the east westwards into the Carnian Alps of Austria. Furthereast they extend beneath the Tertiary sediments of the Pannonianbasin into Hungary. The Karavanke mountains represent a boundaryzone between the Eastern Alps to the north and the Julian and Savinja-Kamnik Alps or Southern Alps to the south. The Periadriatic lineamentintersects the eastern part of the Karavanke mountains fromAustria, trending eastwards, dividing this unit into the Northern andSouthern Karavanke.Geologically, the Karavanke mountains consist of Palaeozoic,Mesozoic (moslly Triassic) rocks and Tertiary sediments. In the eastern part of the Karavanke mountains, along the Periadriatic lineament,there is a belt of magmatic rocks, granite in the north andtonalite in the south, with a narrow belt of metamorphic rocks inbetween.The tectonic structure of the aforementioned boundary zone isespecially interesting. New research res ull~ show that both the overallstructure (1I1d individual tectonic units respectively of this zonesleeply deep towards the south beneath the Julian and Savinja (Kamnik)Alps. The Karavanke mountains are on the north thrusted overEastern Alps by horizontal movements along sing le faults. Amongthese faults, the Pe riadriatic lineament. along which he mentionedmagmatic (granitc - tonalite) zone appears, is especially interesting.This paper attempts 10 define the seq uencc o f tectonic movementswhich took place at the end of lhe Alpine geotectonic cycle,and lhe tectonic structure or the Karavanke M1. zone.
Olševa consists of highly pervious carbonates, forming a relatively big fractured and karstified aquifer. Due to its high-altitude mountainous nature, the aquifer is unpolluted and therefore has to ...be regarded as a potential source of drinking water for the future.The Olševa aquifer is tectonically divided into three parts. Groundwater from the two smaller aquifers, covering areas of 1,9 and 0,8 km2, located in eastern part of Ol{eva massif, flows toward Northeast into Meža river basin. In spite of several transversal faults, the rest of Olševa massif forms a relatively uniform aquifer that is conveying groundwater in westerly direction towards Rjavica valley. Rjavica valley in Austria represents the discharge area of a majority of groundwater from the main Ol{eva aquifer.
The Periadriatic lineament extends from the Sesia zone in Italy across southern Austria into Slovenia, in the area of the Karavanke mountains. It continues eastwards into the Pannonian basin in ...Hungary as the Balaton line. The Karavanke mountain range runs from Slovenia in the east westwards into the Carnian Alps of Austria. Further east they extend beneath the Tertiary sediments of the Pannonian basin into Hungary. The Karavanke mountains represent a boundary zone between the Eastern Alps to the north and the Julian and Savinja-Kamnik Alps or Southern Alps to the south. The Periadriatic lineament intersects the eastern part of the Karavanke mountains from Austria, trending eastwards, dividing this unit into the Northern and Southern Karavanke.
Geologically, the Karavanke mountains consist of Palaeozoic, Mesozoic (mostly Triassic) rocks and Tertiary sediments. In the eastern part of the Karavanke mountains, along the Periadriatic lineament, there is a belt of magmatic rocks, granite in the north and tonalite in the south, with a narrow belt of metamorphic rocks in between.
The tectonic structure of the aforementioned boundary zone is especially interesting. New research results show that both the overall structure and individual tectonic units respectively of this zone steeply deep towards the south beneath the Julian and Savinja (Kamnik) Alps. The Karavanke mountains are on the north thrusted over Eastern Alps by horizontal movements along single faults. Among these faults, the Periadriatic lineament, along which the mentioned magmatic (granite - tonalite) zone appears, is especially interesting.
This paper attempts to define the sequence of tectonic movements which took place at the end of the Alpine geotectonic cycle, and the tectonic structure of the Karavanke Mt. zone.
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