Fig. 8From: Detailed geometry of the subducting Indian Plate beneath the Burma Plate and subcrustal seismicity in the Burma Plate derived from joint hypocenter relocation(a) Map showing the distribution of shallow earthquakes with focal depths less than 50 km. Iso-depth contours are shown for the upper surface of the seismic plane (numbers indicate depth in kilometers). (b) Cross-section along line A–B in the northern area (23.3°–25.0°N). Also shown are earthquakes at depths greater than or equal to 50 km. (c) Cross-section along the line C–D in the central area (21.7°–23.3°N). (d) Cross-section along the line E–F in the southern area (20.1°–21.7°N). Arrows indicate subcrustal earthquakes with E-W P -axes. Z60: the location of the 60-km iso-depth contour. SF: Sagaing Fault.Back to article page