Geological Structure of the Divača Area and its Influence on Kačna Cave Speleogenesis and Hydrogeology
Caves develop along sedimentary and tectonic discontinuities within soluble rock mass. In the Slovene Classical Kras (Karst), the primary lithologies are limestone and dolomite. Previous research of cave systems in SW Slovenia indicated a clear relationship between cave channel directions with local...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Slovenian Academy of Sciences and Arts
2015-12-01
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| Series: | Acta Carsologica |
| Online Access: | https://ojs.zrc-sazu.si/carsologica/article/view/1958 |