GEOLOGY OF THE PENGKALAN HULU-BETONG TRANSECT ...
GEOLOGY OF THE PENGKALAN HULU-BETONG TRANSECT ...
GEOLOGY OF THE PENGKALAN HULU-BETONG TRANSECT ...
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Transect area. In the central part of the Transect area, the rock shows generally dipping<br />
both eastward and westward, with N-S and NE-SW trending directions and well<br />
developed S1 cleavage. The total thickness of the Carboniferous rocks from the<br />
representative section is exceeded 800 m.<br />
The Kubang Pasu/Yaha Formation (Ckp/yh) on the Thai side is distinguishable into two<br />
facies: arenaceous facies (Cyh1) and argillaceous facies (Cyh2).<br />
A<br />
C<br />
Figure 13: Photographs showing the successions of the Kubang Pasu/Yaha Formation<br />
(Ckp/yh) in the southern part of the area (Thai side).<br />
A- Thick bedded sandstone.<br />
B- Chert beds.<br />
C – D- Sandstones in the lowermost unit (Ckp/yh1)<br />
B<br />
D