It can be concluded that: presently the eastern segment of Qilianshan fault zone and its boundary region with Zhuanglanghe fault and Haiyuan fault is in an obvious background of strain accumulation; Lanzhou and Linxia area near the southern segment of Zhu
It can be concluded that: presently the eastern segment of Qilianshan fault zone and its boundary region with Zhuanglanghe fault and Haiyuan fault is in an obvious background of strain accumulation; Lanzhou and Linxia area near the southern segment of Zhu
分析结果表明：祁连山构造带东段及与庄浪河断裂、海原断裂交汇区域目前可能具有相对高应变能积累背景；而庄浪河断裂南段的兰州、临夏一带反映一定程度的应变积累特性。