Upper crustal stress and seismotectonics of the Garhwal Himalaya using small-to-moderate earthquakes: Implications to the local structures and free fluids
Earthquakes in Garhwal Himalaya are related to the Mid-Crustal-Ramp of detachment. NE-SW trending maximum compressive stress is a driving force. Active faults in Chamoli have decreasing frictional strength. Free fluids penetrating around Chamoli region are decreasing the fault strength.