Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6445060 | Journal of Structural Geology | 2013 | 93 Pages |
Abstract
We report new deformation temperature and flow vorticity data from the base of the Greater Himalayan Series (GHS) exposed in the Sutlej Valley and Shimla Klippe of NW India. We focus on three groups of transects across the hanging wall of the Main Central Thrust (MCT). In order of relative foreland - hinterland positions, they are the Shimla Klippe, Western and Eastern Sutlej transects. Deformation temperatures indicated by quartz c-axis fabric opening-angles increase both from foreland to hinterland at a given structural distance above the MCT and up structural section from the MCT within individual transects. Deformation temperatures in the immediate hanging wall to the MCT are estimated at â¼510-535, 535-550 and 610 °C on the Shimla, Western Sutlej and Eastern Sutlej transects, respectively. The steepest inferred field gradients in deformation temperatures are recorded adjacent to the MCT and progressively decrease up structural section following a power law relationship. Comparison with temperature estimates based on multi-mineral phase equilibria data suggests that penetrative shearing occurred at close to peak metamorphic conditions. Vorticity analyses indicate that shearing along the base of the GHS occurred under sub-simple shear conditions (Wm values of 0.9-1.0) with a minor component of pure shear.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
R.D. Law, D.W. III, M.K. Francsis, K.T. Ashley, B. Grasemann, T. Ahmad,