Source Description of the 1999 Hector Mine, California, Earthquake, Part I: Wavelet Domain Inversion Theory and Resolution Analysis

By Chen Ji, David J. Wald, D. Helmberger. 2002

572 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/93356bd585eea14d89362b2952e8fe45fe5b6455

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In Geophysics

Citations in the corpus

The 2005, Mw 7.6 Kashmir earthquake: Sub-pixel correlation of ASTER images and seismic waveforms analysis (2006, methodology): “We have determined a finite source model from the modeling of teleseismic waveforms, in the 0.01– 1H z frequency band, following the procedure of Ji et al. [ 15 ].”
The 2012 Brawley swarm triggered by injection-induced aseismic slip (2015, methodology): “On each subfault, we simultaneously invert for slip, rake, rise time and average rupture velocity using a simulated annealing algorithm (Ji et al., 2002).”
Forecasting the evolution of seismicity in southern California : Animations built on earthquake stress transfer : Stress transfer, earthquake triggering, and time-dependent seismic hazard (2005, background): “... 1992 M = 6.2 Joshua Tree: 1 patch [Ammon et al., 1993; Savage et al., 1993]; 28 June 1992 M = 7.3 Landers: 41 patches, simplified from Wald and Heaton [1994], with Iron Ridge and Argos Mountain faults [Hudnut et al., 1994; Hudnut and Larsen, 1993; Peltzer et al., 1998] added; 28 June 1992 M = 6.”
Accounting for prediction uncertainty when inferring subsurface fault slip (2014, methodology): “Indeed, in most source inversion problems (e.g. Hartzell & Heaton 1983; Delouis et al. 2000; Ji et al. 2002; Simons et al. 2011; Minson et al. 2013, 2014), the discrepancies between data dobs and forward predictions g(̃, m) for a source model m are quantified by defining a least-squares misfit…”
Uncertainties in Finite-Fault Slip Inversions: To What Extent to Believe? (A Critical Review) (2003, unknown): “Li, X., V. F. Cormier, and M. N. Toksöz (2002).”
Simulations of Ground Motion in the Los Angeles Basin Based upon the Spectral-Element Method (2004, background): “Complications associated with source complexity and directivity for larger events (e.g., Wald et al., 1996; Ji et al., 2002) are avoided.”
Numerical Simulation of the 2011 Tohoku Tsunami Based on a New Transient FEM Co-seismic Source: Comparison to Far- and Near-Field Observations (2013, methodology): “For the time-dependent triggering of this source, the risetime computations are based on an asymmetric cosine parameterization, described by JI et al. (2002).”
Depth‐integrated, non‐hydrostatic model with grid nesting for tsunami generation, propagation, and run‐up (2010, background): “[24] and estimated the fault parameters, such as depth, orientation, and slip over 420 subfaults of 6 km by 6 km each.”