摘要
文章通过实测航磁ΔT三维梯度数据与与由航磁ΔT换算出的三维梯度数据的比较,找出其差异,并解释了引起差异的原因。得出在我国目前技术条件下,在需要用航磁ΔT三维梯度数据时,只需实测航磁ΔT的横向水平梯度,其余2个方向梯度值可用由ΔT值换算得出,即可达到解释要求。
Data of the measured 3-dimension △T gradient of air magnetic survey and data of conversion of the 3-dimension AT gradient are compared and difference is shown then causes of the difference are explained and the conclusion is made that under current technical condition if data of the 3-dimension △T gradient are needed only the traverse horizontal gradient is measured the gradient of other two directions could be obtained by conversion that would meet deeds of interpretation.
出处
《地质找矿论丛》
CAS
CSCD
2013年第2期297-300,共4页
Contributions to Geology and Mineral Resources Research
基金
2009年度国家科技支撑计划项目(编号:2009BAB43B01)资助
关键词
航磁异常
航磁ΔT三维梯度
航磁ΔT垂直梯度
航磁ΔT横向水平梯度
航磁ΔT纵向水平梯度
air magnetic anomly
3-dimension △T gradient of air magnetic survey
vertical air magnetic △T gradient
traverse horizontal air magnetic AT gradient
The longitudinal air magnetic △T gradient