The dislocation existed not only in the center part of macroseismic epicenter of the earthquake in 1536 but also near the center of Shaercun village.

• 它不仅存在于1536年强震宏观破坏高烈度区中部，而且还在近中部的沙尔村发现左旋水平扭错约千米左右的次级冲沟。