Application of transient electromagnetic method to detect near surface loess layer in Western China
The topography of the foreland thrust zone in western China is complicated.In those areas, the mountains are steep and the loess layer is thick, which cause the quality of seismic data in these areas is poor.With continuous research in recent years, the quality of seismic data has been improved to some extent.However, it is still difficult to identify the structural traps and build accurate velocity model.It has received a better exploration results on the recognition of loess characteristics and distribution with transient electromagnetic method in the foreland thrust zone.In this paper, the achievement of detecting near surface loess layer in western China using transient electromagnetic exploration is shown.It can be combined with micro-logging to provide the basis for building shallow velocity model for the static correction of the seismic data.
transient electromagnetic loess layer shallow velocity model
Zuzhi Hu Xiangyun Hu Zhanxiang He Zhongcheng Jiang Dechun Li Yunjian Yang Shujiang Yang
Institute of Geophysics and Geomatics China University of Geosciences(Wuhan) Wuhan, Hubei BGP, CNPC Zhuozhou, Hebei
国际会议
北京
英文
379-380
2016-06-27(万方平台首次上网日期,不代表论文的发表时间)