Depositional patterns and structural styles-Hackberry Salt Dome, Cameron Parish, Louisiana
- Amoco Production Co., Houston, TX (United States)
The West and East Hackberry fields of north-central Cameron Parish, Louisiana, are associated with a large southeast-plunging salt ridge. Episodes of salt movement influenced the depositional patterns and reservoir trap styles of the Oligocene- and Miocene-age sedimentary section. The Oligocene lower Hackberry channels were influenced by the salt structure, resulting in the Manchester-Holmwood channel system flanking the east and south sides of the salt dome and the Choupique channel system flanking the west side of the salt dome. The depositional patterns and structural bed dips of the younger Oligocene Camerina A to marginulina section demonstrate a major period of salt movement and erosion. The resulting truncation of the Camerian A sandstones, sealed by overlying shales, provides the dominant trap style for the majority of the reservoirs. This same general period of salt movement influenced the orientation of the Oligocene Marginulina to Miogypsinoides expansion fault system to the east. The Sweet Lake salt dome, down through to this expansion system, probably represents a southeast extension of this ancestral salt ridge.
- OSTI ID:
- 45218
- Report Number(s):
- CONF-941065-; TRN: 95:001437-0041
- Resource Relation:
- Conference: 44. annual convention of the Gulf Coast Association of Geological Societies and the 41st annual convention of the Gulf Coast Section of the Society of Economic Paleontologists and Mineralogists, Austin, TX (United States), 5-7 Oct 1994; Other Information: PBD: 1994; Related Information: Is Part Of Gulf Coast Association of Geological Societies: Transactions. Volume 44; Major, R.P. [ed.]; PB: 847 p.
- Country of Publication:
- United States
- Language:
- English
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