Modulation of Crustal and Mantle Flow Systems by a Cratonic Root in NE Tibet and Western North China Craton: Evidence From Seismic Azimuthal Anisotropy Analysis
The northeastern Tibetan Plateau (TP) and the western North China Craton (NCC) provide a natural laboratory for studying the interaction of tectonic and mantle processes, contrasting the active plateau with the stable craton. In contrast to many prior studies that relied on station‐averaged shear‐wave splitting (SWS) m...