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。

youdao

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。

youdao

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。

youdao