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。
Lanzhou and Linxia area near the southern segment of Zhuanglanghe fault display a feature of strain accumulation in certain degree.
形变分析结果表明，鲜水河断裂带北段处于蠕动状态，南段则处于应变积累的闭锁状态。
The results of deformation analysis show that the north of Xiansuihe fault zone is in creep and that the south of the fault zone is in locking with strain accumulation.
为了获得足够的应变积累来克服动态再结晶的临界应变，低温大变形量的变形是基本条件。
Lowering temperature window of rolling and large strain accumulation is basic condition for exceeding of critical strain for dynamic recrystallization to refine austenite grain size.
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