2017
DOI: 10.1088/1755-1315/88/1/012018
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Analysis on the overpressure characterization with respect to depositional environment facies: Case Study in Miri Area, Baram Delta

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“…It is known that overpressure is mainly generated by under compaction due to the fast rate of deposition of less permeable shales in many tertiary basins [6]. However, two types of overpressure mechanisms were suggested in the study area; the disequilibrium compaction in the pro-delta shales, and fluid expansion in the outer shelf of the region [11]. [12].…”
Section: B Distribution Of Overpressure In the Study Areamentioning
confidence: 91%
“…It is known that overpressure is mainly generated by under compaction due to the fast rate of deposition of less permeable shales in many tertiary basins [6]. However, two types of overpressure mechanisms were suggested in the study area; the disequilibrium compaction in the pro-delta shales, and fluid expansion in the outer shelf of the region [11]. [12].…”
Section: B Distribution Of Overpressure In the Study Areamentioning
confidence: 91%