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本文概括地论述了我省新生代以来主要盆地.断裂的展布形态,活动历史及地壳应力场的作用方式,并探讨了未来破坏性地震危险区.
This article summarizes the main basins in Cenozoic since the Cenozoic in our country, the distribution pattern of fracture, the history of activity and the action mode of crustal stress field, and explores the future destructive earthquake risk zone.