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The term "slip partitioning" is used to describe oblique motion along a fault system that is accommodated on two or more faults with different mechanisms (Fitch 1972; McCaffrey 1992; Jones and Wesnousky 1992; Bowman et al. 2003).
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As the result, the measured distribution of vitrinite reflectance is reasonably fitted with heat generation rate ( left(dot{Q}right) ) and slip duration (t r ) of 16,600 J/s/m2 and 6,250 s, respectively, for the megasplay and 23,200 J/s/m2 and 2,350 s, respectively, for the frontal décollement, implying slow and long-term slips.
But it would be a mistake to write off Jordan for a short-term slip.
The Futagawa segment has 0.2 m/kyr of dextral long-term slip rate and 0.1 0.3 m/kyr of vertical long-term slip rate, and paleoseismological studies indicate that its latest rupture event occurred 2200 6900 years ago.
The fault is loaded by prescribing a long-term slip rate V pl = V 0 near the periodic boundary.
We use the lateral displacement of river channels incised into the Ranau Tuff to constrain the long-term slip rate of two segments of the Sumatran Fault.
Thus, the contributions of tides to long-term slip rates are effectively smaller, despite their larger amplitudes over shorter periods (1 2 kPa).
Using the similar approach, the long-term slip rate estimated from this single river offset is therefore 6.8 ± 1.8 mm/year.
Fault A was located at depths of 30 40 km, similar to the depths where the long-term slip acceleration was dominant (Mavrommatis et al. 2014).
I assume that earthquakes accommodate the bulk of the slip and the elastic constants do not vary greatly so that moment release rate scales with the potency rate obtained from the long-term slip on faults.
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