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The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
Abstract
Chapter from:
Hydrocarbon
Environments
Edited by
Chapter 13
Abnormal Pressure and the Occurrence of Hydrocarbons in Offshore Eastern
Trinidad, West Indies
H.S. Cander
E.B. Eggertson
Amoco Corporation, Houston, Texas, U.S.A.
Abstract
migration
from
thick, Upper Cretaceous source rocks and secondary
migration
through the thick Tertiary
clastics occurred principally through hydraulically induced fractures within a highly
overpressured section. Final
migration
out of the overpressured section and charging of
present-day reservoirs off the
east
coast of Trinidad occurred during the late Pliocene
to Pleistocene uplift and associated complex normal faulting. The multiple pressure
compartments within the six fields studied are separated by relatively thin, abnormally
pressured shale. The shale seals are most effective in trapping hydrocarbons when the
pressure difference across the shale is less than 4 psi/ft (90 kPa/m) regardless of the
shale thickness. Normal faults form effective pressure seals throughout the basin,
separating porous sandstone pressure compartments with pressure differences as great as
1,856 psi (12.8 MPa). The oil and gas fields of offshore Trinidad reveal a widely varying
depth to the top of abnormal pressure, large pressure differences across faults, pressure
reversals, and a narrow zone of transition from mild abnormal pressure (<11 PPG
[lb/gal] equivalent) to highly overpressured conditions (>14 PPG equivalent).
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