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PETROLEUM POTENTIAL

The JDA is geologically located in the North Malay Basin in the offshore lower part of the Gulf of Thailand. The North Malay Basin is a Neogene intracratonic rift/sag basin, elongated in shape, oriented in the northwest-southeast direction and consists of provinces of margin platform, margin ramps and central basinal area or depocentre. Geochemical studies indicate a rich source potential for gas and also for substantial amount of oil. Hydrocarbons within the Malay Basin are found in all of the above provinces. Generally, the North Malay Basin contains thick sediments in excess of 8 km deposited since the Oligocene. Tecto-stratigraphically, the basin is divisible into a Pre-, Syn-, and Post-rift Megasequence. The Megasequence is further divisible into Upper and Lower Post-Rift Megasequence and in some cases in the north divisible into Regional Sagging Megasequence.


Structure Element of the JDA
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Stratigraphic play concept is another potential play but has not been tested yet. Such play type is expected to align along the basin margins at shallow depth updip from the basin depocentre. In the western margin platform province this stratigraphic play looks promising with supporting amplitude anomalies. Early migrated hydrocarbon could be preserved and trapped in this shallow sequence which also has a low geothermal gradient.
 
The structural styles in the JDA are controlled by the movement of normal faults, both pure extensional and transpressional tectonics. The extensional tectonics during Oligocene and Early Miocene caused tilted fault blocks, horst and graben features and anticlinal features against faults. The trap style is mainly fault dependent while widespread marine shales provide a good regional top seal. The intraformational shale in the prospective sequence also provides a very good top seal for individual reservoir package.
Tectonostratigraphy in the JDA
 (click image to view larger image)
 
 
 
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