Ripple mark styles in the Belait Formation: Implications on depositional history.
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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| Main Authors: | , , , , |
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| Format: | Conference or Workshop Item |
| Published: |
2010
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| Subjects: | |
| Online Access: | http://eprints.utp.edu.my/5746/1/Eswaran_Manuscript_NGC2010.pdf http://eprints.utp.edu.my/5746/ |
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