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We use a vertically stratified and laterally homogeneous crust model in this study.
As describes above, the results of the current calculation support the fluid crust model and the crustal shortening model.
This is consistent with the crustal shortening model and the fluid crust model of the uplifting of the LMS.
This study recommends a uplifting mechanism of the LMS, which combines the crustal shortening model and the fluid crust model.
(4) The fluid crust model (Fig. 1d) shows the fluid Tibetan crust flowing over a rigid substrate of the Sichuan Basin (Copley and McKenzie 2007).
In our study, postseismic deformation derived from continuous GPS observations was inverted for optimal smoothed afterslip based on a homogeneous elastic half-space crust model.
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In such regions, it is important to obtain the sediment information (e.g., using an airgun) in addition to data from the global crust models.
The crust layer effect is uniform in oceans and is not very sensitive to difference in thickness as shown in Fig. 6; therefore, the global crust models such as CRUST1.0 (Laske et al. 2013) and CRUST2.0 (Bassin et al. 2000) are useful.
The attenuation function for a laterally homogeneous flat-crust model is also shown (green circles).
Thus, after crossing the crustal barrier, the strain energy of the Lg wave drops to 10% of the flat-crust model at the distance of 1,500 km.
We also examine Lg wave attenuation based on an FDM simulation using a uniform 35-km-thick crust (flat-crust model) as a reference.
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