T343 Continental and Marine Fold and Thrust Belts II
Thursday, 9 October 2008
8:00 AM - 12:00 PM
The Geometry and Kinematics of the Darjeeling - Sikkim Himalaya, India
Paper number: T343-8
Program: Technical Sessions
Time: 9:50 AM – 10:05 AM
Authors
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Gautam MitraUniversity of Rochester, Rochester, NY
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Malay MukulCSIR Centre for Mathematical Modelling and Computer Simulation, Bangalore, N/A
Abstract
We have used INDEPTH geophysical data, the template constraint and return to regional dip arguments to constrain the depth to basal detachment, which varies from ~5 km at the mountain front to ~9 km under the Rangit duplex to ~13 km under the MCT1 and MCT2 ramps; the regional detachment dip is ~3°. Using this in combination with surface structures we have constructed a regional balanced cross section across the DSH. Minimum restorations suggest that the MCT1 and MCT2 sheets have each been translated ~100 km southward. In addition, the RT sheet has been translated ~50 km, and the MBT a minimum of 28 km. Including shortening within the Rangit duplex we estimate a total minimum regional shortening of ~350 km.