Table 1 Misfit statistics between model prediction at GPS sites and GPS data. The latter are derived from Liang et al.45
From: Normal faulting and viscous buckling in the Tibetan Plateau induced by a weak lower crust
Model | RMSmisfit | WRMSmisfit |
|---|---|---|
No weak lower crust | 6.43 | 4.78 |
1021 Pa·s lower crust | 6.07 | 4.51 |
1020 Pa·s lower crust | 5.19 | 3.86 |
1019 Pa·s lower crust | 4.80 | 3.57 |
Case 1-block (three viscosities) | 7.42 | 4.62 |
Case 2-block (four viscosities) | 6.82 | 4.25 |
Thinner weak lower crust | 5.00 | 3.09 |
