Late miocene ostracodes of Serbia: Morphologic and palaeoenvironmental considerations
About 11.5 million years ago, a tectonic uplift of the Eastern and Western Carpathians separated the Pannonian Basin from the rest of the Paratethys. This orogenesis event caused an unconformity between the Sarmatian brackish sediments and the Pannonian lake-sea deposits. More than 6 Ma later, in th...
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| Format: | Article |
| Language: | English |
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Faculty of Mining and Geology, Belgrade
2006-01-01
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| Series: | Geološki Anali Balkanskoga Poluostrva |
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| Online Access: | http://www.doiserbia.nb.rs/img/doi/0350-0608/2006/0350-06080667089R.pdf |