Qinling latitudinal structural belt is developed very clear on the surface, and extends to a certain depth.
秦岭纬向构造带不仅在地表发育明显，而且延伸至地幔一定深度。
The result showed that the illuminated weighting imaging results by wave equation prestack depth migration from relief surface very coincide with the structural configuration of model.
结果表明：起伏地表波动方程叠前深度偏移照明加权成像结果与理论模型构造形态非常吻合。
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