Figure 2
Maps of the true slip-rate distribution every 4 d from the start of the transient to its end. The event nucleates near the southern downdip edge of the fault and propagates updip and to the North.
Maps of the true slip-rate distribution every 4 d from the start of the transient to its end. The event nucleates near the southern downdip edge of the fault and propagates updip and to the North.
