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The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
Abstract
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Chapter 14
Abnormally High Formation Pressures, Potwar
Plateau, Pakistan
B.E. Law1
U.S. Geological Survey, Denver, Colorado, U.S.A.
1Present
Affiliation: Consulting Petroleum Geologist, Lakewood, Colorado, U.S.A.
S.H.A. Shah
M.A. Malik
Oil and Gas Development Corp. of Pakistan, Islamabad, Pakistan
Abstract
drilling
problems
associated with
high pressures have, in some cases, prevented adequate evaluation of reservoirs and
significantly increased
drilling
costs. Previous investigations of abnormal pressure in
the Potwar Plateau have only identified abnormal pressures in Neogene rocks. We have
identified two distinct pressure regimes in this Himalayan foreland fold and thrust belt
basin: one in Neogene rocks and another in pre-Neogene rocks. Pore pressures in Neogene
rocks are as high as lithostatic and are interpreted to be due to tectonic compression and
compaction disequilibrium associated with high rates of sedimentation. Pore pressure
gradients in pre-Neogene rocks are generally less than those in Neogene rocks, commonly
ranging from 0.5 to 0.7 psi/ft (11.3 to 15.8 kPa/m) and are most likely due to a
combination of tectonic compression and hydrocarbon generation. The top of abnormally high
pressure is highly variable and doesn't appear to be related to any specific lithologic
seal. Consequently, attempts to predict the depth to the top of overpressure prior to
drilling
are precluded.
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