JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114, B01315, doi:10.1029/2008JB005746, 2009
Auxiliary material for this article contains illustrations of a synthetic test to the inversion algorithm, the complete kinematic rupture models for the 2004 Mw 6 Parkfield earthquake inferred from inversion of GPS data only, strong motion data only, and combination of GPS and strong motion data, and also a test to the resolving ability of risetimes.
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Figure S1
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Caption: Synthetic test of the two-step combined inversion.
Figure S2
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Caption: Synthetic test: Horizontal GPS static offsets: synthetic data and predicted by the best inferred rupture model.
Figure S3
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Caption: Strong-motion velocity waveforms corresponding to the synthetic test: fault-normal (230°), fault-parallel (140°), and vertical components of motion.
Figure S4
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Caption: Slip amplitude distribution inferred from the GPS-only inversion.
Figure S5
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Caption: Rupture model inferred from the strong motion inversion.
Figure S6
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Caption: Rupture model inferred from the two-step combined inversion using an irregular grid.
Figure S7
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Caption: Test with constrained risetimes: Slip amplitude and 1-s rupture time contours inferred from the two-step combined inversion using an irregular grid.
Table S1
Size: 16 KB
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Caption: Average rupture model obtained from the two-step combined inversion of GPS and strong-motion data using an irregular grid.
Table S2
Size: 16 KB
Format: TXT
Caption: Minimum misfit rupture model obtained from the two-step combined inversion of GPS and strong motion data using an irregular grid.

Citation: (2009), Constraining earthquake source inversions with GPS data: 2. A two-step approach to combine seismic and geodetic data sets, J. Geophys. Res., 114, B01315, doi:10.1029/2008JB005746.