FABRIC ANOMALY IN MUD CLAST DISTRIBUTION IN THE LAMBIR FORMATION (MID TO LATE MIOCENE), SARAWAK.
There is an increasing interest in the anisotropy of mudstone systems mainly due to seismic anisotropy caused by change in wave velocity and polarization with propagation direction. Therefore, the study was to evaluate the variability in the mud clast distribution in the heterolithic sequences prese...
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| Main Authors: | , |
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| Format: | Conference or Workshop Item |
| Published: |
2011
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| Subjects: | |
| Online Access: | http://eprints.utp.edu.my/3931/1/Fabric_Anomaly_Eswaran.pdf http://eprints.utp.edu.my/3931/ |
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