Ripple Mark Styles in the Belait Formation

Ripple Mark Styles in the Belait Formation

The Belait Formation comprises alternating sandstones, sand and clays in varying proportions and thickness and is believed to have been deposited as an isolated basin infilling oscillating between littoral and deltaic-paralic type. Ripples are occasionally encountered in this Formation. However, the...

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Bibliographic Details
Main Authors: Padmanabhan, E., Mohd Pauzi, A.S., Masnan, M.S., Mokhtar, M.A, Prasanna, Mohan Viswanathan
Other Authors: PERSATUAN GEOLOGI MALAYSIA, Geological Society of Malaysia
Format: Conference Paper
Published: Geological Society of Malaysia 2010
Subjects:
stratal architecture
microfacies
paleocurrent
ripples
Belait Formation
Online Access:http://hdl.handle.net/20.500.11937/29187

Internet

http://hdl.handle.net/20.500.11937/29187

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