Data for CPD inversion

This file includes the Curie Point Depth (CPD) model and related data files for the manuscript 'A continental model of Curie Point Depth for China and surroundings based on Equivalent Source Method'<br> This work is fulfilled by Lei, Y., Jiao, L., Huang, Q., and Tu, J.<br> For any questions, please contact us by Email: [e-mail]; [e-mail] The file cpd_result.xyz is the result of the inverted CPD in mainland China, which is shown in Figure 4a. The files *.mat are data complied in Matlab. d_obs.mat is the observed magnetic data from EMM2017, and magnetic responses generated by global oceanic lithospheric magnetization have been removed. <br> ini_cpd.mat is the initial CPD model proposed by Li et al., (2017). <br> Outside the study area, the magnetization is refered to Hemant &amp; Maus, 2005, the magnetic responses are saved as mag_out.mat. The global lithospheric magnetic field model and core field model used in this paper are from EMM2017 and IGRF13, the coeficient file and calculation software are available at https://geomag.us/models/index.html. The global oceanic lithospheric magnetization model is from Masterton et al., (2013). <br> The global vertical integral susceptibility model is from Hemant &amp; Maus, 2005. <br> The global topography data are from ETOPO global relief model, which can be found at https://www.ncei.noaa.gov/products/etopo-global-relief-model<br> The Crust1.0 model are from https://igppweb.ucsd.edu/~gabi/crust1.html. <br> The surface heat flow data are from http://www.ihfc-iugg.org/products/global-heat-flow-database. <br> The radiogenic heat production data are from Sun et al., (2022), and can be found at https://zenodo.org/record/6459746. <br> The CPD model drived from Li et al., (2017) and Gard et al., (2021) can be found in their papers.