琼山区
- 网络Qiongshan District
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利用1605年琼山地震区已有的浅部地质、物探和钻井等资料,采用空间域三维重力正反演计算,消除了地壳浅部影响,依次得到由浅到深的各剩余深部重力异常值。
Using the method of 3-dimension forward calculation in spatial field to eliminate the gravity contributions of shallow crust with data of geology , geophysical prospect and drilling , the different deep residue gravitational anomalies from shallow to deep layer were obtained in turn .