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The AAPG/Datapages Combined Publications Database
AAPG Bulletin
Abstract
AAPG FOUNDATION PRATT CONFERENCE: PETROLEUM PROVINCES,
21st CENTURY
January 12-15, 2000
San Diego, California
Potential
of the Northeast Sakhalin
Shelf
A backarc basin formed in the Oligocene in response to subduction along
the Japan and Kuril arcs. During a period of relative tectonic quiescence,
remnant Paleogene tectonic relief focused paleo-Amur River sedimentation
into major delta systems, represented by the Miocene Dagi and Miocene-Pliocene
Nutovo formations. Basin subsidence was interrupted in Late Pliocene-Early
Pleistocene by a transpressional event generating the large anticlines
which now constitute the major present-day traps of the Sakhalin shelf.
Seismic stratigraphy documents early eastward progradation of Dagi shallow
marine deltaics followed by aggradation and retrogradation, and defines
a similar eastward progradation of the Nutovo delta. Stacked, reservoir
quality Dagi and Nutovo sands on the western shelf represent highstand
stream mouth bar/delta front deposits. Dagi and Nutovo reservoirs are prolific,
with gas test rates up to 160 MMCFD, and oil test rates up to 12,000 BOPD.
The high
fields
total approximately
3 BBO and 30 TCF. Undiscovered
potential
could exceed the discovered volume.
The framework of hydrocarbon accumulations over the present-day shelf reflects
the relationship between tectonics, eustacy, and migrating fluvial-deltaic
depocenters.
potential
future exploration arena is located on the eastern
shelf, where numerous large, untested Dagi and Nutovo structural traps
are present which are analogous to the adjacent discoveries.