Quasi-P wave forward modeling in viscoelastic VTI media in frequency-space domain

被引:18
作者
Li Gui-Hua [1 ]
Feng Jian-Guo [1 ]
Zhu Guang-Ming [2 ]
机构
[1] Shandong Univ Sci & Technol, Shandong Prov Key Lab Deposit Mineralizat & Sedim, Coll Geol Sci & Engn, Qingdao 266510, Peoples R China
[2] Changan Univ, Coll Geol Engn & Geomat, Xian 710054, Peoples R China
来源
CHINESE JOURNAL OF GEOPHYSICS-CHINESE EDITION | 2011年 / 54卷 / 01期
关键词
Forward modeling; Frequency-space domain; Anisotropic; Viscoelastic; Quasi P-wave; FINITE-DIFFERENCE; SCALAR; EXTRAPOLATOR; EQUATIONS; FIELD;
D O I
10.3969/j.issn.0001-5733.2011.01.021
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
The finite difference is an important method of wavefield numerical simulation. It can calculate recursively by time slice, and the round-off errors of each time slice may accumulate to the next time slice in time domain, eventually, which will lead to too large accumulated error when the time slice is enough. However, solving all equation set in frequency domain is based on the frequency slice on the space grid, whose error is assigned to each grid point, it is without accumulated error and easier to simulate the attenuation of the viscoelastic anisotropic media in frequency-space domain. In order to overcome the numerical dispersion of routine finite-difference operators, 25-point optimized finite-difference operators are applied. This paper derives firstly the formula of quasi-P wave in viscoelastic VTI media in frequency-space domain, and then constructs the difference format using 25-point optimized finite difference operators, so it implements forward modeling. A case study of fault model compares and analyzes the crosswell seismic quasi-P wavefield stimulated with the finite difference method for both elastic VTI media and viscoelastic VTI media. In the end, it comes to the conclusion that the amplitude of seismic wave is relatively smaller and the main frequency is decreased in viscoelastic media.
引用
收藏
页码:200 / 207
页数:8
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