后者为斜交东西向构造的断裂、隆坳和褶皱，并与四川盆地西部和荥经地区的北东向构造相连，构成龙门山推覆构造外缘带。
They join with the structures in the west of Sichuan Basin and Rongjing area, and compose the outer edge zone of Longmenshan.
后者为斜交东西向构造的断裂、隆坳和褶皱，并与四川盆地西部和荥经地区的北东向构造相连，构成龙门山推覆构造外缘带。
They join with the structures in the west of Sichuan Basin and Rongjing area, and compose the outer edge zone of Longmenshan.
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