沙丘内部发育有高角度板状交错层理、低角度楔状交错层理等层理构造。
High Angle tabular cross bedding and low Angle wedge cross bedding are generally found on the cross section of the dunes.
沙丘内部发育有高角度板状交错层理、低角度楔状交错层理等层理构造。
High Angle tabular cross bedding and low Angle wedge cross bedding are generally found on the cross section of the dunes.
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