A structural model for the South Tibetan detachment system in northwestern Bhutan from integration of temperature, fabric, strain, and kinematic data

Despite playing a fundamental role in all models of Himalayan tectonics, minimal data constraining the structural evolution, metamorphic history, and offset magnitude of the South Tibetan detachment system (STDS) are available. Here, we integrate petrofabric, finite strain, and kinematic data with metamorphic and deformation temperatures to generate a structural model for the STDS in northwestern Bhutan. We divide the STDS into an similar to 2-km-thick lower level that accommodated similar to 6-13 km of thinning via >= 30-76 km of simple shear-dominant displacement within Greater Himalayan rocks, and an similar to 3-km-thick upper level that accommodated >= 21 km of displacement via an upward decrease (from 44% to 2%) in transport-parallel lengthening within Tethyan Himalayan rocks. Peak metamorphic temperatures in the lower level are similar to 650-750 degrees C, and two distinct intervals of telescoped isotherms in the upper level define a cumulative upward decrease from similar to 700 to similar to 325 degrees C. These intervals are separated by an abrupt upward increase from similar to 450 to similar to 620 degrees C, which we interpret as the result of post-STDS thrust repetition. Above the upper telescoped interval, temperatures gradually decrease upward from similar to 325 to similar to 250 degrees C through a 7-km-thick section of overlying Tethyan Himalayan rocks. Telescoped isotherms lie entirely above the high-strain lower level of the STDS zone, which we attribute to progressive elevation of isotherms during protracted intrusion of granite sills. This study demonstrates the utility of using gradients in fabric intensity and thin section-scale finite strain to delineate shear zone boundaries when field criteria for delineating strain gradients are not apparent.