Model for unstable shelf data sequence, example from a giant south Louisiana discovery - South Lake Arthur field

Conference · Tue May 01 00:00:00 EDT 1990 · AAPG Bulletin (American Association of Petroleum Geologists); (USA)

OSTI ID:6682104

Saxena, R S ^[1]

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1. GEO Consultants International, Inc., Kenner, LA (USA)

In onshore southern Louisiana, exploration emphasis has now shifted to deeper plays in interdomal areas as the majority of the domes have been discovered. Unstable shelf deltas develop in such areas. Several discoveries have been made during the past few years. One giant discovery is South Lake Arthur field, which ideally fits the unstable shelf delta model. Unstable shelf deltas are deep buried structures of very large magnitude in which thick reservoir sandstones are deposited on extensive organic-rich prodelta shales (excellent source rocks). Deposition of reservoir sandstones generates the trapping structures - growth fault and rollover anticline. The sequence is sealed on top by large thicknesses of shales rich in marine organisms. Shelf delta sequences build in localized basins on the part of the shelf that gives actively through combined effects of subsidence, shale compaction, and shale flowage. Sequences develop in stratigraphic units where a strong regressive episode of deposition is immediately followed by a large marine transgression. South Lake Arthur field is a giant gas field discovery with potential reserves in excess of 1 tcf gas. More than 25 wells have been drilled in the field and both the log and the seismic data display the typical unstable shelf delta sequence - 400- to 800-ft-thick reservoir sandstones of Oligocene age - sandwiched between greater than 2,000 ft of prodelta shales at the bottom and 4,000 ft or more of transgressive marine shales at the top. Production is between 17,000 to 18,000 ft. The field is bounded by an arcuate down to the basin fault on the north and is surrounded by shale and salt diapirs. Productive Miogyp sands were deposited in three separate depositional episodes. Lower and middle Miogyp members are thick in the middle part of the field and are dominantly of distributary mouth bar origin - rapidly deposited, poorly sorted, and very shaly.

• OSTI ID: 6682104
• Report Number(s): CONF-900605-; CODEN: AABUD
• Journal Information: AAPG Bulletin (American Association of Petroleum Geologists); (USA), Vol. 74:5; Conference: Annual convention and exposition of the American Association of Petroleum Geologists, San Francisco, CA (USA), 3-6 Jun 1990; ISSN 0149-1423
• Country of Publication: United States
• Language: English

Related Subjects

02 PETROLEUM
58 GEOSCIENCES
LOUISIANA
PETROLEUM DEPOSITS
EXPLORATION
GEOLOGIC FAULTS
GEOLOGIC MODELS
RESERVOIR ROCK
SALT DEPOSITS
SANDSTONES
SEISMIC SURVEYS
SHALES
TERTIARY PERIOD
CENOZOIC ERA
FEDERAL REGION VI
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
GEOPHYSICAL SURVEYS
MINERAL RESOURCES
NORTH AMERICA
RESOURCES
ROCKS
SEDIMENTARY ROCKS
SURVEYS
USA
020200* - Petroleum- Reserves
Geology
& Exploration
580000 - Geosciences