“…A north-south striking normal fault northwest of Pinal de Amoles with a morphologically pronounced fault scarp, 45 km long, likely was the source of the 1887 event (Suter et al, 1996, their Figure 2). An earthquake sequence in 2010-2011, located just south of the trace of this fault, yielded focal mechanisms indicating a north-south striking normal fault as source (Clemente-Chávez et al, 2013). The northern margin of the TMVB is located~60 km south of Pinal de Amoles, where north striking normal faults of the Basin and Range Province are intersected by east-west striking normal faults of the Aljibes half-graben (Suter et al, 1995).…”