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Creator:: Qayyum, Mazhar
Abstract:: The Salt Range is clearly the active participant in the scenario of the progressive southward migration of the Himalayan thrust front. It extends approximately 180 km ENE along strike and is underlain by salt. This is manifested by its very narrow (<1°) cross-sectional taper and great (150 km) width. Integration...
Resource Type:: Masters Thesis

Creator:: Baker, Dan M.
Abstract:: The Salt Range and Potwar Plateau are part of the currently active foreland fold-thrust belt of the Himalaya in Pakistan. Seismic reflection data have been combined with surface mapping, drillhole and paleomagnetic information to construct balanced structural cross-sections of the current frontal thrust zone (Salt Range), and to estimate the...
Resource Type:: Masters Thesis
Full Text:: BIBLIOGRAPHY 90 APPENDICES 101 (A) Development of the Himalayan Frontal Thrust Zone: Salt Range, Pakistan 101

Creator:: Jaswal, Tariq Majeed
Abstract:: The North Potwar Deformed Zone (NPDZ) is part of the active foreland fold-and- thrust belt of the Salt Range and Potwar Plateau (SR/PP) in northern Pakistan. About 500 km of seismic reflection profiles are integrated with surface geologic and drilling data to examine the structure of the NPDZ, in general,...
Resource Type:: Masters Thesis
Full Text:: Potwar Deformed Zone (NPDZ) is part of the active foreland fold- and-thrust belt of the Salt Range and

Creator:: Leathers, Michael R.
Abstract:: The Salt Range and Potwar Plateau of northern Pakistan are part of the thin-skinned, active thrust system related to the ongoing collision of the Asian and Indian continental blocks. Platform rocks and orogenic molasse of the Indo-Pakistani shield are deformed in south-verging thrusts and folds, relative to a northward-converging basement....
Resource Type:: Masters Thesis

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