Abstract:Research purposes: In railway exploration process,we are often caught by bad geological factors such as goaf,softlayer,etc. Under these unfavorable geological conditions,the seismic imaging method is an effective exploration method. The complexity of subsurface collection determines the complexity of the seismic wave field. The difficult of data interpretation and anomaly discrimination leads to the method fails sometimes. To differentiate effective signal and inter- ference signals can improves the accuracy of data interpretation.
Research conclusions:With the actual physical parameters,we effectively simulated the seismic imaging profile. On modeling profile,we can see a significant geophysical anomaly,effectively reflecting the complex structure of the wave field in the shape and characteristics. The finite - difference numerical simulation method allows speed to change vertical- ly and laterally,and better used on actual model. It’s effective for modeling common - offset profile. Through research, we can more accurately determine the anomaly location and shape,and improve the exploring precision. It has a certain significance to the interpretation of actual work.
Xiong Zhangqiang,Zhang Xueqiang,etc. Method of High - density Seismic Imaging Exploration and Application Smaples[J]. Acta Seismologica Sinica,2004(3):313 - 317.
[2] 徐贵来. 地震映像勘探技术研究[J]. 世界核地质科学, 2006(1):33 - 37.
Xu Guilai. Technical Development of Seismic Imaging Prospecting[J]. World Nuclear Geoscience,2006 ( 1 ): 33 - 37.
Zhang Zhifu,Cheng Zhiping. Application of Geophysical Methods in Exploring Karst Structure[J]. Journal of Guilin Institute of Technology ,2003(1):41 -45.
[4] Alford R M. Accuracy of Finite Difference Modeling of Theacoustic Wave Equation[J]. Geophysics,1974(6):834 - 842.
Dong Liangguo,Ma Zaitian,Cao Jingzhong,etc. AStaggered - grid High - order Difference Method of One -order Elastic Wave Equation[J]. Chinese Journal ofGeophysics,2000(3):411 - 419.
Zhou Xueming,Li Qingchun,Li Zhihua,etc. Research on Staggered - grid High - order Finite - difference Numerical Simulation of Seismic Wave[J]. ChineseJournal of Geophysics ,2011(8):1 - 6.
[7]Chen,Y. H.,Chew,W. C.,and Oristaglio,M. L.Application of Perfectly Matched Layers to theTransient Modeling of Subsurface EM Problems[J].Geophysics,1997(6):1730 - 1736.
[8] Chew,W. C. ,and Weedon,W. H. A 3 - D PerfectlyMatched Medium from Modified Maxwell’s Equationswith Stretched Coordinates[J]. Microwave and OpticalTechnology Letters,1994(13):599 - 604.