The study on the fluctuation of moho in yellow sea and its adjacent area 黄海及邻区莫霍面起伏特征
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The structure also control the formation of large and super - large deposits , which commonly lie in the cross of different directions fractures or contacting belts of different tectonic units . 4 . as a whole , gradient belts of moho discontinuity correspond to rock bodies , the flat area correspond to basement 4 、总体上，莫霍面的陡度带一般与岩体相对应，莫霍面的平缓区与基底具有较好的对应关系，大型、超大型矿床一般分布在莫霍面的陡度带_上。
