Upper Jurassic Carbonate Facies Succession at Breze (Velika Kapela, Croatia)
Environmental differentiation at the end of the Lower Malm, as observed at Breze, was caused by gradual synsedimentary tectonics when the hitherto uniform Adriatic carbonate platform was partly differentiated into two different sedimentary environments. Thus the sunken intraplatform trough of unknow...
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| Format: | Article |
| Language: | English |
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Croatian Geological Survey
2010-11-01
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| Series: | Geologia Croatica |
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| Online Access: | http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/380 |