Electrical Structure of the Lithosphere Beneath the Yunkai Massif, South China: Implications for Lithospheric Alteration and Geothermics

The 3D electrical resistivity structure is derived from the dataset of 62 MT sites using the parallel inversion code ModEM based on the nonlinear conjugate gradient algorithm (Egbert &amp; Kelbert, 2012; Kelbert et al., 2014). The input data in inversion was run with an error floor value of 5% for the anti-diagonal impedance tensor and 10% for the diagonal impedance tensor respectively. The output data is the final 3-D electrical resistivity model and model response data.<br>