Data for: Seismic anisotropy beneath the eastern margin of the Tibetan Plateau from SKS splitting observations

This study collects a nearly uniformly distributed seismic array of 512 stations, consisting of four sub-arrays as color-coded in Fig. 1b. Among them, 249 stations are from the Chuanxi Array deployed from October 2006 to July 2009 (Liu et al., 2014); 99 are from permanent China National-backbone stations with data corrected from 2013 to 2017; 168 are from the ChinArray deployed from 2013 to 2016; 25 are from a mobile broadband seismic array deployed in the SCB from 2014 to 2016 by our own research group.