Three-dimensional S-wave azimuthal anisotropy reveals mantle flows in the central and eastern North China CratonOA

The subduction and rollback of the Western Pacific Plate and expansion of the Qinghai-Xizang Plateau have significantly influenced the tectonic evolution of the North China Craton(NCC).However,the detailed characteristics of the associated deep dynamic processes remain poorly understood.Seismic anisotropy serves as a key indicator for probing deformation and dynamics in the interior of the Earth.Based on surface wave data recorded by dense seismic arrays,this study applied the Eikonal tomography method to obtain Rayleigh-wave azimuthal anisotropy images at periods of 12–120 s across the central and eastern NCC.We further inverted these data to create a three-dimensional(3D)shear-wave velocity structure and azimuthal anisotropy to a depth of 260 km.Our results revealed a prominent low-velocity anomaly in the upper mantle beneath the centraleastern study region,where the fast direction is primarily E-W.We suggest that this low-velocity anomaly likely originated from the dehydration of the stagnant Western Pacific slab in the upper mantle,which induces partial melting that subsequently ascends to the base of the lithosphere.Furthermore,the E-W anisotropic pattern is likely associated with eastward asthenospheric flow caused by the retreating subduction of the Pacific Plate.East of the Ordos Block,an N-S trending lowvelocity anomaly below 180 km depth exhibits weak anisotropy,which may be attributed to deep material upwelling associated with eastward asthenospheric flow and abrupt lateral variations in lithospheric thickness.In the northeastern NCC,the fast direction in the asthenosphere and below shifts to NW-SE,which is distinct from that beneath the North China Plain.This difference may reflect variations in the subduction angle and rollback rate between the Japan and Ryukyu trenches.Our findings provide new observational constraints on lithospheric deformation and deep dynamic processes in this region.