Subsurface cavity imaging by crosshole borehole radar measurements

被引:53
作者
Zhou, H [1 ]
Sato, M
机构
[1] Ocean Univ China, Coll Marine Geosci, Qingdao 266003, Peoples R China
[2] Nagasaki Univ, Fac Engn, Dept Elect & Elect Engn, Nagasaki 8528521, Japan
[3] Tohoku Univ, Ctr NE Asian Studies, Sendai, Miyagi 9808576, Japan
来源
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING | 2004年 / 42卷 / 02期
基金
中国国家自然科学基金; 日本学术振兴会;
关键词
borehole radar; cavity detection; combination of tomography and migration; reverse-time migration; tomography;
D O I
10.1109/TGRS.2003.817215
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Travel time tomography uses direct waves of crosshole radar data. A great deal of information concerning the media is contained in later arrivals, such as reflections and diffractions. More reliable results can be obtained by incorporating both direct waves and later arrivals. In this paper, the combination of travel time tomography and migration is introduced. A smoothed velocity model obtained by travel time tomography is used as the basis of migration. Then, a reverse-time migration technique is applied to direct-wave-suppressed crosshole data. The result of tomography indicates that there is an abnormal area, and the result of migration gives a more accurate position of the abnormal area, which is a cavity. The real example shows that the cooperation of tomography and migration is an effective technique for subsurface-cavity imaging. The synthesis of all information, including parallel crosshole measurement and forward simulation, assists in the interpretation of the results of tomography and migration.
引用
收藏
页码:335 / 341
页数:7
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