Fig. 5From: Unraveling the role played by a buried mud diapir: alternative model for 2016 Mw 6.4 MeiNong earthquake in southwestern Taiwana Coseismic dilatational strain at depth of 1.4 km. An unclamping region (positive value) matched our sill model (black rectangle). The gray rectangle with red edge is the main fault plane from Lee et al. (2016). b The locations of north–south and east–west planes above the main fault. c and d Are different view angles for static normal stress changes on these planesBack to article page