It considers transient frequency constraints, transient voltage-dip constraints, steady-state voltage constraints, and CLPU characteristics using a modified bisection algorithm.
Thus, the use of a full 3D model including such heterogeneities as described above is necessary to provide depth and dip angle constraints for offshore earthquakes in the subduction zone.
Additionally, the bootstrapping results may eventually be used to incorporate a priori knowledge of the fault plane orientation (in particular dip) in providing better constraints on the moment magnitude for shallow earthquakes.
This level of accuracy in relative depth is not high enough to provide good constraints on the dip angle of the fault plane.
Without a third component of the displacement and geometric constraints on the dip of the faults, we cannot make a quantitative comparison between horizontal and vertical slip values collected in the field and our offsets.
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Local animal health infrastructure constraints included livestock dips (used to control external parasites such as ticks) in need of structural repair and also the limited numbers of dips serving a large pastoralist population.
The obtained displacement field is consistent with a right-lateral motion along the Hinagu fault, and thus, the rake was assumed to be a right-lateral with no constraint on dip-slip orientation.
We here demonstrate a simple mechanical model of faulting in elastic half-space from Okada (1992) with several constraints from field observations and estimated fault dip at depth.
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However, several geodynamic scenarii have been proposed for its formation including a south or a north dipping subduction, which are still debated due to lack of constraints.
