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...
Saved in:
Main Authors: | Padmanabhan, Eswaran, Mohd Pauzi, Ahmad Syabil |
---|---|
Format: | Conference or Workshop Item |
Published: |
2011
|
Subjects: | |
Online Access: | http://eprints.utp.edu.my/3931/1/Fabric_Anomaly_Eswaran.pdf http://eprints.utp.edu.my/3931/ |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Fabric variability within layered Fe-oxide deposits in Mid-Late Miocene sedimentary formations, NW Borneo: Impact on facies architectural interpretations
by: Padmanabhan, Eswaran, et al.
Published: (2008) -
Spatial – Temporal Variability of Hydrocarbon Distribution in the Lambir Formation, NE Sarawak
by: Ramli, Syamim, et al.
Published: (2012) -
SOME DIFFERENTIATING FIELD CHARACTERISTICS BETWEEN THE BELAIT & LAMBIR FORMATIONS, NORTH SARAWAK.
by: Ramli, Mohd Syamim, et al.
Published: (2011) -
Sedimentology Stratigraphy and Microfossils of Mid – Late Tertiary Clastic, Sandakan Formation in NE Borneo
by: Chow Weng Sum, Chow
Published: (2012) -
Geochemistry of Miocene sedimentary rocks from offshore West Baram Delta, Sarawak Basin, Malaysia, South China Sea: implications for weathering, provenance, tectonic setting, paleoclimate and paleoenvironment of deposition
by: Padmanabhan, Eswaran
Published: (2017)