2002
DOI: 10.3133/ofr9950t
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Petroleum systems of the Malay Basin Province, Malaysia

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Cited by 15 publications
(27 citation statements)
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“…The source rocks in the Malay Basin are overmature in the centre due to deep burial and high geothermal gradients generally ranging from $45 to 60 1C/km (Madon, 2007). In the southern part of the basin, gradients as low as 36 1C/km have been reported by Bishop (2002). Most gas fields are related to overmature coaly source rocks in the depocentre, whereas oilfields towards the margin of the southeastern Malaysian part of the basin are related to lacustrine source rocks within the oil generation window .…”
Section: Petroleum Geology Of the Malay Basinmentioning
confidence: 98%
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“…The source rocks in the Malay Basin are overmature in the centre due to deep burial and high geothermal gradients generally ranging from $45 to 60 1C/km (Madon, 2007). In the southern part of the basin, gradients as low as 36 1C/km have been reported by Bishop (2002). Most gas fields are related to overmature coaly source rocks in the depocentre, whereas oilfields towards the margin of the southeastern Malaysian part of the basin are related to lacustrine source rocks within the oil generation window .…”
Section: Petroleum Geology Of the Malay Basinmentioning
confidence: 98%
“…), and the basin consists of a complex of grabens and half-grabens mainly filled with Paleogene-Neogene lacustrine mudstones, continental siliciclastic rocks, and coaly strata. In the deepest central part, the sediment fill is more than 14 km thick (Bishop, 2002;Madon, 2007). High burial and sedimentation rates in the early syn-rift phase caused overpressure in the basin, which is presently characterised by a domal overpressure distribution with the top of overpressure occurring at $2 km depth in the basin centre and deeper at the basin margins (Madon, 2007).…”
Section: Petroleum Geology Of the Malay Basinmentioning
confidence: 98%
See 2 more Smart Citations
“…It is an elongated NW-SE intracontinental extensional basin (500 x 250km) and covers a total area of ca. 80,000km 2 [1,2]. Since 1970's, exploration efforts in the Malay Basin were directed towards the more obvious structural traps such as compressional anticlines and fault-dip closures.…”
Section: Introductionmentioning
confidence: 99%