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References in periodicals archive ?
In the immediate footwall of the Main Central thrust, peak temperatures average 550 degrees C.
An inverted thermal field gradient of - 20 degrees C/km is also documented beneath a klippe of the Main Central thrust hanging wall - 25 km south of the Vaikrita thrust, and a peak footwall temperature of 530 degrees C is recorded close to the shear zone at the base of the klippe.
The age differences in samples from northern and southern exposures are interpreted to document cooling related to thermal relaxation following passage of the Main Central thrust hanging wall atop the Lesser Himalayan Sequence.
The Main Central Thrust Zone (MCTZ) has been studied along several sections in western Nepal, Dolpo region.
P-T conditions have been constrained using geothermobarometers in high temperature mylonites while to constraint the P-T conditions during the ductile to brittle tectonic evolution of the MCTZ zone fluid inclusion analyses have been performed on quartz lenses from kyanite bearing gneisses and micaschists sampled from the Main Central Thrust Zone and in quartz inclusions trapped in garnet crystals.
The HHC forms the hanging wall of the Main Central Thrust (MCT) and incorporates pelitic, psammitic and quartzite sequences together with thin amphibolite and calc-silicate bands along with granitoids of various ages.
GHS rocks in the Sutlej Valley, NW India, are exposed in an ~16 km thick panel, bounded below by the Main Central thrust (MCT) and above by the Sangla Detachment, a local strand of the South Tibetan Detachment system (STDS) of normal faults.
However, because the top-to-the-north and top-to-the-south shear fabrics are predominant in the north- dipping Main Central thrust (MCT) below and the South Tibet detachment (STD) above across the entire GHC, the tectonic significance of the orogen-parallel deformation in exhumation of the GHC was often ignored.