Supporting information for "Tectonic strain causes the inclination divergence of paleomagnetic data from the Upper Cretaceous redbeds in the Lhasa Terrane, insight from AMS, hf-AIR and CPO"

The research used anisotropy of magnetic susceptibility (AMS), high-field anisotropy of isothermal magnetic remanence (hf-AIR) and electron backscatter diffraction (EBSD) techniques to study the Shexing Formation redbeds from the Lhasa terrane.