文章摘要
杨生,郭刚.高精度磁测磁异常的计算与理解[J].矿产勘查,2011,2(6):780-783
高精度磁测磁异常的计算与理解
The calculation and understanding of magnetic anomaly in high- accuracy magnetic survey
投稿时间:2011-07-05  
DOI:
中文关键词: 高精度磁测  正常场  异常场  ΔT
英文关键词: high- accuracy magnetic survey  normal field  anomalous field  ΔT
基金项目:
作者单位
杨生 有色金属矿产地质调查中心,北京 100012 
郭刚 有色金属矿产地质调查中心,北京 100012 
摘要点击次数: 2272
全文下载次数: 1364
中文摘要:
      文章根据实测磁场的构成要素直接推出了测点磁异常的计算公式,和以往采用分步改正求取磁异常的方法具有相同的结果。根据矢量运算法则,导出了ΔT和异常场的关系,给出了ΔT的意义,其是磁异常在正常场方向上的分量,正负取决于异常场和正常场的夹角,锐角时为正,钝角时为负。
英文摘要:
      According to the inscape of magnetic field surveyed, the author concludes the calculation formula of magnetic anomaly on the measuring point in this paper. The method mentioned above has clear thinking and clear meaning, meanwhile. It can get the same result with the usual method of correcting and obtaining magnetic anomalies step by step. On the basis of vector algorithms, it is educed the correlation between ΔT and anomalous field. And ΔT is the component of magnetic anomaly in the direction of normal field. It is determined by the included angle between anomalous field and normal field, that ΔT is positive or negative. When the included angle is less than right-angle, ΔT is positive. On the contrary,ΔT is negative.
查看全文   查看/发表评论  下载PDF阅读器
关闭