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Abstract
Chapter from: M
66: Hydrocarbon Migration And Its Near-Surface Expression
Edited By
Dietmar Schumacher and Michael A. AbramsAuthors:
Michael J. Kaluza and Earl H. Doyle Geochemistry, Generation, Migration
Published 1996 as
part of Memoir 66
Copyright © 1996 The American Association of Petroleum
Geologists. All Rights Reserved. |
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Kaluza,
M. J., and E. H. Doyle, 1996, Detecting fluid migration in shallow sediments:
continental slope environment, Gulf of Mexico, in D. Schumacher
and M. A. Abrams, eds., Hydrocarbon migration and its near-surface expression:
AAPG Memoir 66, p. 15-26.
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Chapter
2
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Detecting
Fluid Migration in Shallow Sediments: Continental Slope Environment, Gulf
of Mexico |
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Michael J.
Kaluza
Fugro-McClelland Marine
Geosciences, Inc.
Houston, Texas, U.S.A.
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Earl H. Doyle
Shell Offshore, Inc.
Houston, Texas, U.S.A.
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Abstract
The detection
of shallow gas features on the northern Gulf of Mexico continental slope
has been aided with a unique positively buoyant deep-towed subbottom profiler
and side-scan sonar system. The tool provides high-quality, high-resolution
seismic displays of the shallow (upper 75 m) stratigraphy and seafloor
images (400-m swath) capable of resolving geologic features that may constrain
exploration drilling or engineering development of potential petroleum
reserves.
From the more than 20,000
km (~10,000 nmi) of deep-tow data collected, numerous encounters of shallow
gas features have been made. Gas and other fluid vents have been seen on
the seafloor in association with seafloor and shallow buried fault systems.
In some cases, vents have been identified by distinctive seafloor topography
expressed as hills and mounds and by seafloor depressions, craters, and
blister-like features. No distinctive topographic irregularities occur
at other seafloor vent areas, which are identified primarily by the seismic
character of the records. Shallow subsurface gas has been identified by
the amorphous and wiped-out character of stratified sequences on subbottom
profiler data and by high-amplitude "bright spot" reflections within sediment
packages. Gas flow, both vertically along fault planes and laterally along
permeable sediment layers, can be identified from these types of data. |
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