Fig. 1: Improvements in constraining subsurface coupling using earthquake focal mechanisms. | Nature Communications

Fig. 1: Improvements in constraining subsurface coupling using earthquake focal mechanisms.

From: 3D architecture and complex behavior along the simple central San Andreas fault

Fig. 1

Schematic comparison of data and assumptions used in a previous geodetic inversion studies11,12,13,15 and b this study relying on the spatial distribution of earthquakes and slip directions from focal mechanisms. Dark red areas denote locked patches and light red areas denote creeping areas. Modeled fault c creep rate and d creep direction around a locked patch. Yellow stars and beachballs denote earthquake locations and focal mechanisms, respectively. Black and blue beachballs are on-fault and off-fault earthquakes, respectively. Red arrows show the assumed fault slip direction. Black thin lines in (d) denote local creep directions on the NE side of the fault.

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