In contrast, the subbasins in the stress shadow became inactive and dead as a result strain localization on the linked through-going basin-bounding faults.
与此同时，由于应力逐渐集中在大型次级盆地边界断层之上，处于应力影中的次级盆地停止发育。
The normal residual stress at interface is great, which can result in the interface de-bounding.
界面处残余法向应力较高，可能造成界面脱粘。
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