另外，在强震震中沿活动构造带或沿块体边缘迁移时，迁移时间也有相隔5个月的现象。
In addition, when the epicenters of strong earthquakes migrated along the active tectonic zone or the edge of a block, a 5-month separation for the the migration was also observed.
这项研究成果将为评价龙门山断裂带余震和今后强震发展趋势提供关键构造物理参数。
These results provide key appraisal for future assessments of earthquake hazards of the Longmenshan fault zone and aftershock occurrences.
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