摘要
功率谱方法在磁数据处理方面的应用比较广泛。采用近似公式直接求出地质体的上下底埋深。在此近似方法中,会出现一些影响结果的因素。主要对地质体的水平尺寸和厚度的影响做了一些研究,并得出相应的结论。
Power spectrum method in the application of magnetic data processing is more extensive.This approximate formula is obtained directly by the upper and lower end of the depth of geological bodies.In this approximation,there will be some of the factors that affect the results.In this article,mainly on the level of geological body size and thickness did some research,and draw appropriate conclusions.
出处
《吉林大学学报(地球科学版)》
EI
CAS
CSCD
北大核心
2010年第S1期17-20,共4页
Journal of Jilin University:Earth Science Edition
关键词
功率谱
位场
地质体深度
power spectrum
bit field
geological depth