Fig. 5From: Activity of crustal faults and the Xolapa sliver motion in Guerrero–Oaxaca forearc of Mexico, from seismic dataSchematic representation of oblique subduction system kinematics. Black line (\(T_\text{n}\))—normal to the trench, blue arrow (\(V_\text{c}\))—convergence velocity vector, orange arrow (\(V_\text{s}\))—coseismic slip vector, green arrow (\(V_\text{ss}\))—strike-slip component, \(\gamma\)—convergence obliquity, \(\psi\)—subduction obliquityBack to article page