Growth history and facies evolution of the subis limestone - A carbonate platform exposed onshore Borneo Island, Malaysia
The Subis Limestone is a Member of the Tangap Formation. It is Upper Oligocene to Lower Miocene in age. The Subis Limestone is divided into two sequences which are different in depositional setting and architecture. The lower sequence is Upper Oligocene in age, generally deep marine depositional env...
| Main Authors: | , , |
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| Format: | Conference Paper |
| Published: |
European Association of Geoscientists and Engineers, EAGE
2013
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| Online Access: | http://hdl.handle.net/20.500.11937/15308 |