Structural styles of the High Atlas mountains, Morocco: Potential hydrocarbon traps in the footwall of thrusts developed from the reactivation of syn-rift normal faults
Conference
·
· AAPG Bulletin
OSTI ID:6861788
- Inst. for the Study of Continents, Ithaca, NY (United States); and others
Large asymmetrical folds and box folds created by fault bend and fault propagation folding characterize the style of deformation in the High Atlas mountains. Several compressional phases of faulting and folding from the Lower Jurassic through Cenozoic indicate a long and varied tectonic origin for the High Atlas intracontinental mountain belt. Footwall shortcut faults are formed with the inversion of syn-rift listric: normal faults, and progress into low angle thrust faults with fault bend fold geometries. This style of deformation is illustrated on reprocessed seismic reflection data and confirmed by field mapping. Geological field mapping, air photographs, and Thematic Mapper imagery provide important constraints for the interpretation of seismic reflection profiles along the margins of the High Atlas mountains. Balanced cross sections across the High Atlas suggest large horizontal displacements along low angle thrust faults. These thrusts place massive Lower Jurassic carbonates above post-rift Upper Cretaceous and Tertiary rocks. Refolding of thrusts and large scale regional folds indicate oblique slip deformation during and after the inversion of syn-rift normal faults. Low angle thrusts propagate along detachments in shales and marts of the Lower Jurassic. Lower Jurassic shales provide an excellent seal for potential sandstone reservoirs in the Middle Jurassic and Triassic sandstones in the footwall of thrusts.
- OSTI ID:
- 6861788
- Report Number(s):
- CONF-960527--
- Conference Information:
- Journal Name: AAPG Bulletin Journal Volume: 5
- Country of Publication:
- United States
- Language:
- English
Similar Records
Structural styles of the High Atlas mountains, Morocco: Potential hydrocarbon traps in the footwall of thrusts developed from the reactivation of syn-rift normal faults
Intracontinental rifting and inversion: Missour basin and Atlas Mountains, Morocco
Deformation in footwall of Clinchport thrust, valley and ridge of northwest Georgia
Conference
·
Mon Dec 30 23:00:00 EST 1996
·
OSTI ID:425421
Intracontinental rifting and inversion: Missour basin and Atlas Mountains, Morocco
Journal Article
·
Sun Sep 01 00:00:00 EDT 1996
· AAPG Bulletin
·
OSTI ID:411873
Deformation in footwall of Clinchport thrust, valley and ridge of northwest Georgia
Conference
·
Fri May 01 00:00:00 EDT 1987
· AAPG (Am. Assoc. Pet. Geol.) Bull.; (United States)
·
OSTI ID:6110486