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Limestones of Bukit Biwah and Bukit Taat, Kenyir Lake, Terengganu represent a limestone unit that was deposited during the Middle Permian. The limestone is made up of mudstone, wackestone and packstone with subordinate grainstone. The dominant grains comprise tests and shells of shallow marine organisms that dwelled on the sea bottom during the Permian (algae, foraminifera, bryozoa, fusulines, brachiopod, bivalve, gastropod and coral). Some other grains are made up of peloidal material. The rock has undergone several diagenetic processes including surface or near surface cementation when the sediment was at the sea bottom and also late burial cementation. Apart from that dolomitization seems to be very common though not pervasive. The presence of minor low amplitude stylolites and dissolution seams indicate that the rock unit has not experienced extreme pressure and deformation.

Fasies karbonat dan diagenesis di dalam batu kapur Bukit Biwah dan Bukit Taat, Kenyir, Ulu Terengganu