Development of the Himalayan frontal thrust zone: Salt Range, Pakistan
Journal Article
·
· Geology; (United States)
The Salt Range is the active frontal thrust zone of the Himalaya in Pakistan. Seismic reflection data show that a 1 km offset of the basement acted as a buttress that caused the central Salt Range-Potwar Plateau thrust sheet to ramp to the surface, exposing Mesozoic and Paleozoic strata. The frontal part of the thrust sheet was folded passively as it overrode the subthrust surface on a ductile layer of Eocambrian salt. Lack of internal deformation of the rear part of the thrust sheet is due to decoupling of sediments from the basement along this salt layer. Early to middle Pliocene (approx. 4.5 Ma) conglomerate deposition in the southern Potwar Plateau, previously interpreted in terms of compressional deformation, may instead document uplift related to basement normal faulting. Stratigraphic evidence, paleomagnetic dating of unconformities, and sediment-accumulation rates suggest that the thrust sheet began to override the basement offset from 2.1 to 1.6 Ma. Cross-section balancing demonstrates at least 20 to 23 km of shortening across the ramp. The rate of Himalayan convergence that can be attributed to underthrusting of Indian basement beneath sediments in the Pakistan foreland is therefore at least 9-14 mm/yr, about 20-35% of the total plate convergence rate.
- Research Organization:
- Oregon State Univ., Corvallis (USA)
- OSTI ID:
- 5334343
- Journal Information:
- Geology; (United States), Journal Name: Geology; (United States) Vol. 16:1; ISSN GLGYB
- Country of Publication:
- United States
- Language:
- English
Similar Records
Interpretation of seismic reflection data across the Himalayan foreland thrust belt in Pakistan
Structure and evolution of the northern Potwar deformed zone, Pakistan
Strike-slip faulting in a foreland fold-thrust belt, western Salt Range, central Pakistan
Conference
·
Mon Dec 31 23:00:00 EST 1984
· Geol. Soc. Am., Abstr. Programs; (United States)
·
OSTI ID:6197395
Structure and evolution of the northern Potwar deformed zone, Pakistan
Journal Article
·
Fri Jan 31 23:00:00 EST 1997
· AAPG Bulletin
·
OSTI ID:437309
Strike-slip faulting in a foreland fold-thrust belt, western Salt Range, central Pakistan
Conference
·
Mon Dec 31 23:00:00 EST 1984
· Geol. Soc. Am., Abstr. Programs; (United States)
·
OSTI ID:6319372
Related Subjects
58 GEOSCIENCES
580201* -- Geophysics-- Seismology & Tectonics-- (1980-1989)
ASIA
BASEMENT ROCK
DEFORMATION
DEVELOPING COUNTRIES
GEOLOGIC FAULTS
GEOLOGIC FRACTURES
GEOLOGIC HISTORY
GEOLOGIC STRUCTURES
GEOLOGY
GEOPHYSICAL SURVEYS
GROUND UPLIFT
HIMALAYAS
MAGNETISM
MOUNTAINS
PAKISTAN
PALEOMAGNETISM
PLATE TECTONICS
SEDIMENTATION
SEISMIC SURVEYS
STRATIGRAPHY
SURVEYS
TECTONICS
580201* -- Geophysics-- Seismology & Tectonics-- (1980-1989)
ASIA
BASEMENT ROCK
DEFORMATION
DEVELOPING COUNTRIES
GEOLOGIC FAULTS
GEOLOGIC FRACTURES
GEOLOGIC HISTORY
GEOLOGIC STRUCTURES
GEOLOGY
GEOPHYSICAL SURVEYS
GROUND UPLIFT
HIMALAYAS
MAGNETISM
MOUNTAINS
PAKISTAN
PALEOMAGNETISM
PLATE TECTONICS
SEDIMENTATION
SEISMIC SURVEYS
STRATIGRAPHY
SURVEYS
TECTONICS