“我们认为地块可能断裂的最长区段往往是遭受8级地震的地区，”艾伦说。
"We think that the longest sections of the faults that can rupture are equivalent to a magnitude-8 earthquake," says Allen.
活动地块和断裂构成了该区主要的构造框架。
Thus, blocks and faults constitute the main tectonics frame in this zone.
佳木斯地块西缘金矿带是受深断裂控制的，矿床之间是相互联系的，是在一个构造应力体制下完成它们的成矿作用的。
Auriferous belt at western margin of Kiamusze massif is controlled by deep rupture, depositions are correlative. The auriferous belt 's mineralization is finished under same tectonic stress system.
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