“…With Tikhonov regularization, the solution will be at most a flattened and/or smoothed model of the earth's subsurface. Nevertheless, the smooth model is not always the best model for geologic structures that are commonly characterized by sharp boundaries and comprise distinct geologic bodies, for example, the sharp petrophysical boundaries between the host rocks and the hydrocarbon reservoir zones (Michelena and Harris, 1991; boundary-preserving regularizations have been developed in image reconstruction to restore sharp edges and high-contrast images (Charbonnier et al, 1997). Some schemes have been applied to geophysical data, for example, the compactness body constraint (Last and Kubik, 1983;Ajo-Franklin et al, 2007), the L p -norm (Claerbout and Muir, 1973;Bube and Langan, 1997;Farquharson, 2008;Zhang and Castagna, 2011;Li et al, 2012;Zhang et al, 2013), total variation regularization (e.g., Farquharson and Oldenburg, 1998), the minimum gradient constraint (Portniaguine and Zhdanov, 1999;Abubakar et al, 2008), and the level-set method (Lelièvre et al, 2012;Li and Leung, 2013;Zheglova et al, 2013;Li et al, 2014).…”