Hydrologic Evolution of a Carbonate Aquifer (Dinaric Karst, Croatia)
Dinaric Karst terrains contain specific, lam inatedspeleothems, which line all surfaces of subterraneanvoids including Cretaceous bedrock limestone, and oldervadose speleothems and clastic sediments. The speleotherms may attain a thickness of one metre. Deposition of these speleothems took place dur...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Croatian Geological Survey
2010-11-01
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| Series: | Geologia Croatica |
| Online Access: | http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/330 |