摘要
由地震射线和电磁波射线组成的射线层析成像技术(CT)在地学领域已得到了广泛的应用。介绍了地震CT中的一种基于最短走时路径的射线追踪方法;研究了电磁波CT中的井间电磁波场强幅值相对归一化方法。应用表明,上述方法是可行的。
The ray path tomography composed of seismic and electromagnetic waves, is widely used in the geophysical prospecting. A ray path trail method based on the mininum travelling time in the seismic tomography is introduced. And a relative normalized method in finding field intensity amplitude for crosshole electromagnetic wave tomography is researched. Engineering practice showed that the above mentioned methods are feasible.
出处
《长江科学院院报》
EI
CSCD
北大核心
1998年第6期31-33,43,共4页
Journal of Changjiang River Scientific Research Institute
关键词
地震射线
电磁波射线
场强幅值
射线层析成像
seismic tomography
electromagnetic wave tomography
field intensity amplitude
application