Fig. 2From: Aftershock activity of the 2015 Gorkha, Nepal, earthquake determined using the Kathmandu strong motion seismographic arrayHypocenter distribution in Kathmandu region estimated from double-difference hypocenter calculation (Waldhauser and Ellsworth 2000). The cross sections are parallel and perpendicular to the strike of the Himalayan main thrust belt; a dashed line in the right section indicates the Himalayan main thrust. Triangles and solid line indicate seismographic stations and border of the Kathmandu metropolitan area, respectivelyBack to article page