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通过对地球物理场特征与不同层次地质体之间对应关系的分析,可以探讨深层构造的演化。本文根据对重力和磁力场数据处理的结果,研究皖中地区地壳上部的层块结构和滑脱构造。
By analyzing the correspondence between geophysical field features and geologic bodies at different levels, the evolution of deep structures can be explored. Based on the results of gravity and magnetic field data processing, this paper studies the block structure and slippage in the upper crust of Anhui Province.