Ouachita-Appalachian junction: a Paleozoic transpressional zone
Conference
·
· AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
OSTI ID:6254888
The late Paleozoic collision of the Gondwana supercontinent with the trailing southern margin of North America created the Ouachita and Appalachian orogenic belts. Transecting these belts are several transpressional or wrench fault zones, including the Val Verde basin-Texas lineament system, the Ardmore-Anadarko basin trend, and the Reelfoot rift complex. Vertical movement within these wrench zones resulted in the emplacement of pop-block or flower structures. In Texas and Oklahoma these features are major structural traps for oil and gas. In this work, they propose that the (buried) juncture between the Ouachita and Appalachian foldbelts in Mississippi is a similar transpressional fault zone. Recent reconstructions of the collision between Gondwana and North America indicate a relative closure direction of southeast to northwest. Normal decollement thrusting occurred in the Appalachian and Ouachita foldbelts, where the structural grain of the North American margin was nearly perpendicular to the closure direction. Where the structural grain was oblique to closure direction, wrench faulting and high-angle thrust faulting occurred, due to the combined effect of both translational and compressional stress fields. In southwestern Alabama and Mississippi the trailing North American plate margin consisted of Mississippian and Pennsylvanian clastics draped over a thick Cambro-Ordovician carbonate shelf. This shelf trends northeast-southwest in Alabama but turns sharply to trend north-northwest in Mississippi, possibly reflecting changes in Precambrian basement relief. Transpressional stresses would have been generated near this sharp bend during the collision. This study identifies one such transpressional fault zone, on the basis of seismic data and well control, in east-central Mississippi.
- Research Organization:
- Amoco Production Co., New Orleans, LA
- OSTI ID:
- 6254888
- Report Number(s):
- CONF-870606-
- Conference Information:
- Journal Name: AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States) Journal Volume: 71:5
- Country of Publication:
- United States
- Language:
- English
Similar Records
Ouachita-Appalachian juncture: A paleozoic transpressional zone in the Southeastern USA
Influence of a continental promontory on time and place of orogeny
Subsidence history of the Alabama promontory in response to Late Paleozoic Appalachian-Ouachita thrusting
Journal Article
·
Wed Mar 31 23:00:00 EST 1993
· AAPG Bulletin (American Association of Petroleum Geologists); (United States)
·
OSTI ID:6077509
Influence of a continental promontory on time and place of orogeny
Conference
·
Tue Dec 31 23:00:00 EST 1991
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:5688920
Subsidence history of the Alabama promontory in response to Late Paleozoic Appalachian-Ouachita thrusting
Conference
·
Mon Feb 28 23:00:00 EST 1994
· Geological Society of America, Abstracts with Programs; (United States)
·
OSTI ID:7059493
Related Subjects
02 PETROLEUM
020200* -- Petroleum-- Reserves
Geology
& Exploration
ALABAMA
CAMBRIAN PERIOD
CARBONATE ROCKS
EXPLORATION
FEDERAL REGION IV
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC STRUCTURES
MINERAL RESOURCES
MISSISSIPPI
NORTH AMERICA
ORDOVICIAN PERIOD
PALEOZOIC ERA
PETROLEUM DEPOSITS
RESOURCES
ROCKS
SEDIMENTARY BASINS
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TECTONICS
USA
020200* -- Petroleum-- Reserves
Geology
& Exploration
ALABAMA
CAMBRIAN PERIOD
CARBONATE ROCKS
EXPLORATION
FEDERAL REGION IV
GEOLOGIC AGES
GEOLOGIC DEPOSITS
GEOLOGIC STRUCTURES
MINERAL RESOURCES
MISSISSIPPI
NORTH AMERICA
ORDOVICIAN PERIOD
PALEOZOIC ERA
PETROLEUM DEPOSITS
RESOURCES
ROCKS
SEDIMENTARY BASINS
SEDIMENTARY ROCKS
TECTONICS
USA