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. The supporting information file includes:Figure S1. Secondary electrons microscope (SEM) photo (left) and mineral distribution (right) detected by electron backscatter diffraction (EBSD) of representative specimens.Table S1. Field parameters of sampling sites.Data Set S1. The raw data of AMS, hf-AIR and EBSD results.