THE SEDIMENTOLOGY OF HYDROCARBON RESERVOIR ROCKS IN INDONESIA, A CASE STUDY FROM THE NORTH SUMATRA BASIN
DOI:
https://doi.org/10.29017/SCOG.13.1.1126Keywords:
Sedimentology, Hydrocarbon, Reservoir RocksAbstract
The North Sumatra backarc basin has been an important hydrocarbon province for more than 100 yrs. High grade light oils and condensates have been produced from sandstone reservoirs in the deltaic Keutapang Formation and the shallow marine sandstones of the Baong Formation. The basin has a high geothermal gradient, which is in the order of 40-50 C/km (compared to 30/km in the North Sea or Gulf Coast areas) and is a result of its position close to the subducting margin of the Indian Ocean Plate.
References
Bjorlykke, K., 1983. Diagenetic Reactions in Sandstones, pp 169-213 in Parker, A. and Sellwood, B.W. (Eds) Sediment Diagenesis. D. Reidel Publishing Company.
Boles, J.R. and Franks, S.G., 1979. Clay Diagenesis in the Wilcok Sandstones of Southwest Texas: Implications of Smectite Diagenesis on Sandstone Cementation. Journal of Sedimentary Petrology, Vol. 49, pp. 55-70
Curtis, C.D. 1978. Possible Links between Sandstone Diagenesis and Depth Related Geochemical Reactions Occurring in Enclosing Mudstones. Journal of the Geological Society of London, Vol. 135, pp. 107-117.
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