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- W2010916226 abstract "A sensitivity study of stochastic crustal and Moho models on Moho refracted first arrivals is presented. The crustal model is a self-affine velocity structure superposed on a linear velocity gradient. The Moho is represented by a first-order discontinuity with a topography which is also self-affine. The sensitivity of both travel-time and wave-field is considered. We found that the full wave-field around the Pn arrival is sensitive to crustal structures down to 1 km, and to Moho undulations down to 5 km. However, the first arrivals are only sensitive to crustal structure down to about 3 km, and to Moho structure down to 10 km. Our analysis suggests that the wide-angle full wave-field has a sensitivity that is intermediate between the sensitivity of the vertically reflected wave-field and wide-angle arrival times. These findings give some justification to the mainstream ray tracing approach to wide-angle data inversion, where resulting models incorporate only a moderate number of features at relatively large scales." @default.
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- W2010916226 date "1999-08-15" @default.
- W2010916226 modified "2023-09-26" @default.
- W2010916226 title "Sensitivity of seismic wide-angle wave-field and first arrival times to fine scale crustal structure and moho topography" @default.
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- W2010916226 doi "https://doi.org/10.1029/1999gl900553" @default.
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