Upper Cretaceous Gosau deposits of the Apuseni Mountains (Romania) - similarities and differences to the Eastern Alps
The Apuseni Mountains were formed during Late Cretaceous convergence between the Tisia and the Dacia microplates as part of the Alpine orogen. The mountain range comprises a sedimentary succession similar to the Gosau Group of the Eastern Alps. This work focuses on the sedimentological and geodynami...
| Main Authors: | , , , , |
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| Format: | Journal Article |
| Published: |
Austrian Geological Society
2009
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| Online Access: | http://hdl.handle.net/20.500.11937/11517 |