a listric fault has decreasing dip angle with depth forming curved faults, and a detachment fault is a low-angle fault into which many listric faults merge forming a single system

a listric fault has decreasing dip angle with depth forming curved faults, and a detachment fault is the opposite and increases in dip angle with depth

a listric fault has decreasing dip angle with depth forming curved faults, and a detachment fault is a strike-slip fault (same as dextral fault)

a listric fault has increasing dip angle with depth forming curved faults, and a detachment fault detaches the crust from the mantle

a listric fault has increasing dip angle with depth forming curved faults, and a detachment fault is the opposite and decreases in dip angle with depth