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强震通常发生在运动板块的边界地带,但欧亚板块内部却经常出现八级以上的强震活动。这些特殊的板内强震活动,反映了板内破裂构造的特性。它们同板块运动协调一致,密切相关,为认识板内强震活动规律提供了线索。
Strong earthquakes usually occur on the boundary of the moving plate, but strong earthquakes of magnitude eight or more often occur in the Eurasian plate. These special intraplate strong earthquakes reflect the characteristics of intraplate rupture structures. They are closely related to plate movement and closely related, providing clues for understanding the laws of strong earthquakes in plate.