Growth history and facies evolution of the subis limestone - A carbonate platform exposed onshore Borneo Island, Malaysia

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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...

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Bibliographic Details
Main Authors:	Dedeche, A., Pierson, B., Hunter, Aaron
Format:	Conference Paper
Published:	European Association of Geoscientists and Engineers, EAGE 2013
Online Access:	http://hdl.handle.net/20.500.11937/15308

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