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Fluvial reservoir architecture in the Malay Basin: Opportunities and challenges

Conference · · AAPG Bulletin (American Association of Petroleum Geologists); (United States)
OSTI ID:6749865
;  [1]
  1. Esso Production Malaysia Inc., Kuala Lumpur (Malaysia)
Miocene fluvial sandstones are significant hydrocarbon-bearing reservoirs in the Malay Basin. These include high energy, braided stream deposits of group K, associated with late development of extensional half grabens and relatively lower energy, meandering, and anastomosing channel deposits of group I formed during the subsequent basin sag phase. Group K reservoirs are typically massive, commonly tens of meters thick, and cover an extensive part of the Malay Basin. These reservoirs have good porosity and permeability at shallow burial depths. However, reservoir quality deteriorates rapidly with increasing depth. Lateral and vertical reservoir continuity is generally good within a field, commonly forming a single system. Good water drive enhances recovery. Seismic modeling to determine fluid type and the extent of interfluvial shales is possible due to reservoir homogeneity.
OSTI ID:
6749865
Report Number(s):
CONF-940803--
Conference Information:
Journal Name: AAPG Bulletin (American Association of Petroleum Geologists); (United States) Journal Volume: 78:7
Country of Publication:
United States
Language:
English

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