Tectonic Inception in Caledonide Marbles
A fundamental difference between caves in sedimentary limestones and those formed in a repeatedly-glaciated 40000 km2 region in central Scandinavia that contains over 1000 individual marble outcrops and has nearly 1000 recorded karst caves is the metamorphic grade of the karst bedrock and its neglig...
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| Format: | Article |
| Language: | English |
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Slovenian Academy of Sciences and Arts
2006-06-01
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| Series: | Acta Carsologica |
| Online Access: | https://ojs.zrc-sazu.si/carsologica/article/view/239 |