b Inverted slip with respect to the SLAB model.
General features of this display appear similar to Fig. 3(b), though it is clear that the southern edge of the model has lower resolution than the central portion, with standard deviations 60% or more of inverted slip values (i.e. low slip, high standard deviation, vs. <20% near the hypocenter, indicating high slip, low standard deviation).
Fixing these geometrical parameters, we then invert the slip distribution from the GPS data (request for digital slip model should be addressed to F. Diao).
To invert for slip distributions on each segment that are physically plausible, we solve a non-negative least-squares problem that restricts the slip directions together with a constraint on the smoothness of the slip distributions (e.g., Simons et al. 2002, Furuya and Yasuda 2011).
InSAR data are well inverted to slip on the Futagawa and Hinagu faults.
The seismic waves inverted for slip models are usually displacements or velocities filtered in a low-frequency band, which is typically <1 Hz.
Using horizontal GPS velocities between 2013 and 2015 from the latest data of the Crustal Movement Observation Network of China (CMONOC) (Fig. 1a), we inverted the slip rates across the Huya Fault using a profile projection method.
Though there are an articulated type leg and a tail such that the suggested one-legged hopping robot cannot be effectively approximated by the famous Spring Loaded Inverted Pendulum (SLIP) model system, the dynamics of the robot is considerably simplified since the novel design for the body.
Hsu et al. (2012) inverted the slip-deficit rates and the geometric configuration of the southernmost Ryukyu subduction zone.
Fault planes are divided into a series of subfaults along the strike and dip directions, and we invert for the slip amplitude, direction, rise-time and rupture initiation time of each subfault, where subfault source time functions are modeled with an asymmetric cosine function (Ji et al., 2002, 2003).
