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Review of principal hydrocarbon-bearing basins around the South China Sea

1985; Geological Society of Malaysia; Volume: 18; Linguagem: Inglês

10.7186/bgsm18198508

2637-109X

Ernest P. Du Bois,

Methane Hydrates and Related Phenomena

As a consequence of exploration for hydrocarbons, and of research programmes conducted by academic and international institutions, substantial progress has been made in recent years in definition of hydrocarbon-bearing basins, and those potentially so, in southeast Asia and especially in the vicinity of the South China Sea. Basins and depositional provinces now recognized include: the Thai Basin, the Khorat and Panjang Basins, the Malay Basin, West Natuna and Penyu Basins, Saigon (Ho Chi Minh) and Mekong (Vung Tau) Basins, East Natuna area, the Greater Sarawak Basin including Central Luconia and Balingian depositional provinces, the Baram Delta/Brunei-Sabah Basin and the Northwest Palawan Shelf. Where hydrocarbons have been encountered, the deposits are commonly associated with rocks of Middle and Upper Miocene age. Oliogene and Pliocene occurrences are locally significant. With some exceptions, most sedimentary basin-fill was deposited within continental to coastal environments. Such sediments are commonly gas-prone. Where oil-prone, there are suggestions that the oil has been generated under conditions of greater thermal maturity.