Multigeophysical constraints on the extent and mechanisms of lithospheric destruction in the North China Craton

The input data used in our multi-observable probabilistic inversion include Rayleigh wave dispersion curves (phase_dispersion.zip), filtered elevation (elev_China_dat.xyz), filtered geoid height (geoid_China_dat.xyz), and surface heat flow (SHF_2019.txt). 3D thermochemical structure of the whole lithosphere and sublithospheric upper mantle beneath the North China Craton is concluded in Anqi_Zhang_NCC_results.xlsx, including temperature, density, shear wave velocity, depth to the lithosphere-asthenosphere boundary, and magnesium number of the lithospheric mantle.