These evidences prove that the Early and Middle Triassic paralic and lacustrine features had already been inactive in the Middle and Late Triassic Ordos basin.

表明中晚三叠世鄂尔多斯盆地已经结束早中三叠世近海湖泊的性质。

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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。

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