Facies modelling of Ngimbang Clastics interval of Ngimbang formation with the integration of rock physics analysis and simultaneous inversion, North East Java Basin
Penulis/Author
WAHYUNI ANNISA H (1); Prof. Dr. Ir. Sugeng Sapto Surjono, S.T., M.T., IPU., ASEAN.Eng. (2); Dr. Sarju Winardi, S.T., M.T. (3); I Made Sutha Negara (4)
Tanggal/Date
18 2021
Kata Kunci/Keyword
Abstrak/Abstract
The Middle Eocene Ngimbang Clastics interval of the Ngimbang formation represents the oldest syn-rift deposits in the
North East Java extensional basin. It has been proven in previous publications its potential as source rock. Apart from that,
Ngimbang Clastics interval can also potentially be a hydrocarbon reservoir rock. This study enhances the understanding of
facies and sandstone reservoir distribution in this interval, through the analysis of electro-facies, rock physics and simultaneous inversion by using well logs and 3D pre-stack seismic data. Facies map of this interval is generated based on lithology
and fuid impedance for determining reservoir potential area. The results show that three facies types of rock−5000 to 3500
ft/s×g/cc for porous sand, above 4000 to 20,000 ft/s ×g/cc for shaly-sand, shale and non-porous sand and above 20,000
ft/s×g/cc for coal based on the lithology impedance. Reservoir interval is porous sand facies with good porosity of 9.5–
17.5%. Facies development for reservoir distribution in the study area is constructed based on a slicing lithological impedance
map which shows that the porous sand facies are deposited in alluvial-braided channels, and in a wave-dominated estuarine
depositional environments. Porous sand has a geometry of channel flls and bars that develop on the study area’s west and
southwest sides. Gas sand identifed based on fuid impedance has value below 15,500 ft/s×g/cc. The distribution of gas
fuid in the Ngimbang Clastics interval’s porous sandstones can be found on the west and southwest side of the study locally
TURNITIN- Facies modelling of Ngimbang Clastics interval of Ngimbang formation with the integration of rock physics analysis and simultaneous inversion, North East Java Basin_compressed.pdf
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