The authors research the mechanism of indirected display on surface caused by buried geological anomaly at first, on the basis of physical simulated tests.
用物理模拟方法研究隐伏地质异常地表间接显示机理，探讨隐伏线性构造在水平挤压条件下的表面特征。
Before analyzing seismic wave anomaly and velocity profiles. the polarity of reflected signal should be adjusted to be same as the physical significance of reflection coefficient.
在震波异常与速度剖面分析之前。应将反射信号之极性调整到与地层中反射系数之物理意义相一致。
The difference between the lithosome shape, distribution of kimberlite and the physical natures of adjacent rock decides the size, intensity of anomaly and the reflecting degrees.
金伯利岩岩体形状空间分布与围岩的物性差别，决定了异常大小强弱、反映明显程度；
The difference between the lithosome shape, distribution of kimberlite and the physical natures of adjacent rock decides the size, intensity of anomaly and the reflecting degrees.
金伯利岩岩体形状空间分布与围岩的物性差别，决定了异常大小强弱、反映明显程度；
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