Delineating Geothermal Structure from 3D Joint Inversion of MT and Gravity Data
Delineating Geothermal Structure from 3D Joint Inversion of MT and Gravity Data
We have implemented 3D faults as discontinuity surfaces, of finite extent, in the RLM-3D inversion regularization, and used the scheme during both 3D cooperative and cross-gradient joint inversions of geothermal MT and gravity data, firstly for synthetic model, and then for the Sorik Marapi ...