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.

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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.

youdao