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As mentioned before, Δ|T| depends on Φ0 as well as Δ Φ. Parameters in RSF cycle simulations are usually adjusted so as to yield a reasonable stress drop Δ τ of an earthquake cycle.
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The optimized value of stress drop, 64 bars, is reasonable for a large event (Ugurhan and Askan 2010; Zengin and Cakti 2014).
Since these eight Nantou events all ruptured on the buried faults within a small region, it is reasonable to agree with the suggestion of Wen et al. (2014) that the high stress drop of these eight Nantou events might be related to an immature buried fault.
The stress drop is approximately 11 MPa.
Stress drop was scattered around 1 10 MPa.
We determine the stress drop using an optimization algorithm.
Near-complete stress drop would increase the ratio of the stress change to the differential stress, also facilitating stress rotation.
The differences indicate the stress drop of the simulation.
Dashed lines represent constant values of Brune's stress drop.
Further investigation may clarify the depth dependence of stress drop.
The stress drop is a fundamental parameter of earthquake dynamics.
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