Continental Subduction Tectonics in the High Karst Dinarides of Western Croatia
The faults confining Palaeozoic inliers surrounded by Mesozoic rocks, show that their relation is not a consequence of folding but of neotectonic uplift causing a rather uneven relief of the Palaeozoic units underlying the carbonate Mesozoic. The predominance of tectonic contacts indicates that simi...
Main Authors: | , |
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Format: | Article |
Language: | English |
Published: |
Croatian Geological Survey
2010-11-01
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Series: | Geologia Croatica |
Subjects: | |
Online Access: | http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/375 |