Differential strain between both terrains was accommodated across the Wenchuan-Mouwen ShearZone, which developed during D_3 as a sinistral strike-slip zone.
两个地区的差异应变被发育于D_3的汶川-茂汶左行剪切带所容纳。
Differential strain between both terrains was accommodated across the Wenchuan-Mouwen ShearZone, which developed during D_3 as a sinistral strike-slip zone.
两个地区的差异应变被发育于D_3的汶川-茂汶左行剪切带所容纳。
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