Obduction of the lower crust contributing to the uplift of the Longmen Shan revealed by receiver function imaging in eastern Tibet

To investigate the crustal deformation of the Longmenshan region, we imaged the fine crustal structure by using teleseismic P-wave receiver functions (RFs) along a dense nodal seismic array across the LMS and removed the scattered surface waves generated by the steep topography. This folder uploaded includes the raw data used to RFs ('LMS_raw_data_SH_2017_2018_NEZ'), the calculated RFs ('LMS_RFs_SH_2017_2018'), the RFs with removing the topographic scatters ('LMS_RFs_SH_2017_2018_rmsc'), the crustal image data (the common conversion point (CCP) stacking of RFs)('CCP_LMS.txt'), and the crustal image data after removing the topographic scatters ('CCP_LMS_Remove_scatters.txt'). The folders for raw data and RFs are stored according to events, and the files under each event folder start with the station number. The raw data and the RFs are in SAC format.