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