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    In:  J. Geophys. Res., Oxford and Edinburgh, Blackwell Scientific Publications, vol. 111, no. B9, pp. 1-14, pp. B09408, (ISBN: 0534351875, 2nd edition)
    Publication Date: 2006
    Description: The gravity signal contains information regarding changes in density at all depths and can be used as a proxy for the strain accumulation in fault networks. A stress evolution time-dependent model was used to create simulated slip histories over the San Andreas Fault network in California. Using a linear sum of the gravity signals from each fault segment in the model, via coseismic gravity Green's functions, a time-dependent gravity model was created. The steady state gravity from the long-term plate motion generates a signal over 5 years with magnitudes of ...
    Keywords: Gravimetry, Gravitation ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Stress ; Strain ; Modelling ; 1217 ; Geodesy ; and ; Gravity: ; Time ; variable ; gravity ; 7209 ; Seismology: ; Earthquake ; dynamics ; 0515 ; Computational ; Geophysics: ; Cellular ; automata ; 4430 ; Nonlinear ; Geophysics: ; Complex ; systems ; Fernandez
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