摘要
本文采用三维解析信号法研究了青海省旺尕秀地区地磁异常特征。通过对化极磁异常、低通滤波异常等的分析,结合研究区地表地质圈定出了局部磁异常,分析了局部磁异常的成因;采用化极磁异常三维解析信号振幅值和其半宽估算磁源体的埋深。对区内圈定的四处磁源体做了定性定量分析,为本区基础地质研究提供了有力依据。
This paper uses three-dimensional analytic signal method to study geomagnetic anomaly characteristics in the Wang gaxiu area,Qinghai province.Firstly,geomagnetic anomaly to magnetic pole,low-pass filter,to delineate local magnetic anomaly,and finally use the amplitude value of the three-dimensional analytic signal of magnetic anomaly and its half width to estimate the buried depth of the magnetic source.The qualitative and quantitative analysis of the circular magnetic source has provided a strong basis for the basic geological research in this area.And it is found that in the middle and high latitudes,the three-dimensional body anomaly is weakened or disappeared by the 3d analytic signal processing,which indicates that this method is more sensitive to the linear structure,and weaker for the circular structure.
作者
李艳
雷江平
陈武杰
LI Yan;LEI Jiangping;CHEN Wujie(The Bureau of Natural Resources of Hancheng City,Hancheng 715400,China)
出处
《四川有色金属》
2022年第2期27-30,共4页
Sichuan Nonferrous Metals
关键词
中高纬度
磁异常
三维解析信号
the middle and high latitudes
magnetic anomaly
three-dimensional analytical signal