北交图和本命盘在结构特性上单独的比较就已经十分有趣。
The individual comparison between natal and draconic structure patterns also interesting.
其矿床遥感地质影像模式为:受控于北东向和北西向断裂构造交切所夹的环形断块。
The geologic image model of the mineral deposit is annular fault block controlled by northeast and northwest structures.
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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