吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (3): 830-836.doi: 10.13278/j.cnki.jjuese.20180274
张雅晨1,2, 刘财1,2, 陈光宇3
Zhang Yachen1,2, Liu Cai1,2, Chen Guangyu3
摘要: 归一化总梯度法对下半空间的重力总梯度模进行归一化计算,从而利用极值来获得地质体的分布,但现有计算方法存在计算精度较低的问题,并且计算结果不太稳定。本文采用Hartley变换,并引入新的余弦滤波因子,实现重力归一化总梯度,来压制高频干扰;此外,针对计算过程中下延深度越大干扰越严重的弊端,将余弦滤波因子的幂次设计为随深度变化的函数,从而获得更加稳定的计算结果。模型试验和在玲珑金矿区采空区的实际数据结果表明,所提出的重力归一化总梯度法具有计算速度快、精度高、稳定性强等优点。
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