2017
DOI: 10.1007/s13369-017-2867-6
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Comparative Study of Pore Pressure in Wells of Indus Offshore, Southwest Pakistan

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Cited by 2 publications
(6 citation statements)
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“…The seismic reflection profiles near Jal Pari-1A reveal mud diapirism whereas, in the west, it is less observed. Overpressures in the east of Jal Pari-1A, in Indus Marine wells (Indus Marine-1A and Indus Marine-1C) have been previously reported by Khan (2018). According to Khan (2018), the overpressure or high-pressure development in the Indus Marine wells is likely attributable to the high sedimentation rate and disequilibrium compaction during the Neogene (Miocene Epoch).…”
Section: Formation Pressure Evaluationmentioning
confidence: 73%
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“…The seismic reflection profiles near Jal Pari-1A reveal mud diapirism whereas, in the west, it is less observed. Overpressures in the east of Jal Pari-1A, in Indus Marine wells (Indus Marine-1A and Indus Marine-1C) have been previously reported by Khan (2018). According to Khan (2018), the overpressure or high-pressure development in the Indus Marine wells is likely attributable to the high sedimentation rate and disequilibrium compaction during the Neogene (Miocene Epoch).…”
Section: Formation Pressure Evaluationmentioning
confidence: 73%
“…The high-pressure development in this area may likely be attributable to the mud diapirism associated with stratigraphic strata, as shown in Figures 8-11. Overpressure to the east of Jal Pari-1A, in Indus Marine wells, has been reported by Khan (2018). According to Khan (2018), the overpressure or high-pressure development in the Indus Marine wells is likely caused by the high sedimentation rate and disequilibrium compaction during the Miocene Epoch.…”
Section: Discussionmentioning
confidence: 99%
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