Crustal Shortening and Rheological Behavior Across the Longmen Shan Fault, Eastern Margin of the Tibetan Plateau

Knowledge of lithospheric rheology can provide fundamental insights into crustal deformation near the Longmen Shan fault (LMSF). Based on viscoelastic deformation models constrained by interseismic geodetic observations, we obtain an optimal crustal shortening rate of 4.8 +/- 0.4 mm/a across the LMSF and an upper mantle viscosity of 5.0 x 10(20-21) Pa center dot s beneath eastern Tibet. More importantly, we find a high-viscosity zone (>10(21) Pa center dot s) in the lower crust beneath the LMSF, where the steady-state viscosity is significantly higher than the transient viscosity derived from postseismic deformation. Further investigations with a power-law rheology suggest that, due to the stress loading of the Wenchuan earthquake and the relaxation afterwards, the effective lower crustal viscosity decreases to similar to 10(18) Pa center dot s immediately after the earthquake and finally recovers to interseismic level (similar to 10(21) Pa center dot s). Our results highlight the stress-dependent behavior and the viscoelastic effect of rheological structure beneath the LMSF during the earthquake cycle.

Automated summary

Knowledge of lithospheric rheology provides fundamental insights into crustal deformation near the Longmen Shan fault (LMSF). The study reveals a high-viscosity zone beneath the LMSF, where the steady-state viscosity is significantly higher than the transient viscosity. Furthermore, the effective lower crustal viscosity decreases immediately after the earthquake and recovers to interseismic level.