Yushu 2010 earthquake epicenter in the fault zone of discontinuous parts, non-consecutive parts that en echelon strike-slip fault zone is usually a high incidence area of ??seismic activity.

In 2010 an earthquake epicenter-Shee is broken is not continuous with the body, shows that the geese slip-break activities with non-continuous site is usually the high seismic activity.

The eucalyptus in 2010 the earthquake center is in the fault zone not the continual spot, indicated walks in the echelon slides the active fault zone not continual spot is usually the seismic activity succeeding in the imperial civil service examinations region.

2010 yushu earthquake epicenter in discontinuous parts of the fault zone, indicating the Echelon-slip active fault zone of discontinuous parts are usually areas with a high incidence of seismic activity.

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