The formation of the Dabashan orocline, central China: Insights from high-resolution 3D crustal shear-wave velocity structure.

• We developed a joint inversion method by combination of surface-wave dispersions, receiver functions, Ps and SsPmp travel times. • We obtained detailed three-dimensional Vs and Vp/Vs ratio models in the area. • A northeast-dipping low Vs zone is observed in the upper crust of the Dabashan orocline. • We proposed a tectonic model on formation of Dabashan orocline. The Dabashan orocline is a large thrust belt in central China. Determination of its high-resolution three-dimensional (3D) crustal shear-wave (S -wave) velocity structure can enhance our understanding of the intracontinental evolution of the South China plate and North China plate. In this study, we estimated the Rayleigh wave phase and group velocities at periods of 5–50 s, P -wave receiver functions, and Ps and SsPmp travel times from 63 permanent stations and 29 portable stations; we also constructed a 3D S -wave velocity model and crustal thickness and V p / V s ratio maps of the Dabashan orocline and adjacent areas. The crustal thickness and V p / V s ratio maps show prominent thick crust (50–55 km) and high V p / V s ratios (1.8–1.85), suggesting a mafic lower crust in the Dabashan orocline. The 3D S -wave velocity structure shows northeast-dipping low-velocity anomalies in the upper crust of the Dabashan orocline, and high velocities extended from near the surface to the lower crust in the Hannan-Micang and Shennong-Huangling domes, suggesting deep roots of the two domes. We propose that the two domes acted as rigid indenters and rotated clockwise together with the South China plate, penetrating into the Qinling-Dabie orogenic belt. Weak sediments in the upper crust of the Dabashan orocline were compressed and blocked by the two domes and the rigid Qinling-Dabie orogenic belt, resulting in vertical accretion of the sediments and crust and subsequent formation of the northeast-dipping low-velocity anomalies and the thick crust beneath the Dabashan orocline. [ABSTRACT FROM AUTHOR]