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Central Luconia, offshore Sarawak, has long been recognized as a prolific carbonate province with large hydrocarbon reserves. Carbonate reefs growth initiated mainly on structural highs formed during Late Oligocene rifting. The main phase of carbonate growth occurred during the mid to late Miocene (Fig. 1). Some of these carbonate buildups are aerially very extensive and cover several hundred square kilometers. Eustatic sea-level changes during the Miocene influenced the growth rate of, and facies distribution within carbonate build-ups. Recently, with increasing understanding of the Central Luconia carbonate system, a new carbonate sedimentation mechanism has been recognized that of carbonate turbidite deposition. These carbonate turbidites are present in palaeo­ lows between Miocene/Pliocene carbonate platforms.

Seismic interpretation of carbonate turbidites in Central Luconia