Now the inclined plane separates it and makes it into two discontinuous layers. It must be caused by the displacement along the inclined plane.

 
  • 現在傾斜面使這一巖層分開(kāi),使之變成兩個(gè)不連續的巖層,這一定是由于沿著(zhù)傾斜面巖層發(fā)生位移而造成。
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