The One-Way Wave Equation: A Full-Waveform Tool for Modeling Seismic Body Wave Phenomena

被引:16
作者
Angus, D. A. [1 ]
机构
[1] Univ Leeds, Sch Earth & Environm, Leeds, W Yorkshire, England
关键词
Forward modeling; One-way wave equation; Seismic anisotropy; Wave phenomena; FREQUENCY-DEPENDENT ANISOTROPY; ELASTIC-WAVE; SYNTHETIC SEISMOGRAMS; FRACTURE CHARACTERIZATION; DOWNWARD-CONTINUATION; BORN APPROXIMATION; PARABOLIC EQUATION; NARROW-ANGLE; TRAVEL-TIME; RAY THEORY;
D O I
10.1007/s10712-013-9250-2
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 study of seismic body waves is an integral aspect in global, exploration and engineering scale seismology, where the forward modeling of waves is an essential component in seismic interpretation. Forward modeling represents the kernel of both migration and inversion algorithms as the Green's function for wavefield propagation and is also an important diagnostic tool that provides insight into the physics of wave propagation and a means of testing hypotheses inferred from observational data. This paper introduces the one-way wave equation method for modeling seismic wave phenomena and specifically focuses on the so-called operator-root one-way wave equations. To provide some motivation for this approach, this review first summarizes the various approaches in deriving one-way approximations and subsequently discusses several alternative matrix narrow-angle and wide-angle formulations. To demonstrate the key strengths of the one-way approach, results from waveform simulation for global scale shear-wave splitting modeling, reservoir-scale frequency-dependent shear-wave splitting modeling and acoustic waveform modeling in random heterogeneous media are shown. These results highlight the main feature of the one-way wave equation approach in terms of its ability to model gradual vector (for the elastic case) and scalar (for the acoustic case) waveform evolution along the underlying wavefront. Although not strictly an exact solution, the one-way wave equation shows significant advantages (e.g., computational efficiency) for a range of transmitted wave three-dimensional global, exploration and engineering scale applications.
引用
收藏
页码:359 / 393
页数:35
相关论文
共 103 条
[1]  
Al-Anboori ASS, 2005, THESIS U LEEDS
[2]  
Al-Harrasi O, 2010, THESIS U BRISTOL
[3]   Fracture characterization using frequency-dependent shear wave anisotropy analysis of microseismic data [J].
Al-Harrasi, O. H. ;
Kendall, J. -M. ;
Chapman, M. .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2011, 185 (02) :1059-1070
[4]  
ALTERMAN Z, 1968, B SEISMOL SOC AM, V58, P367
[5]  
Angus D, 2007, IMPROVED COMPUTATION
[6]   True amplitude corrections for a narrow-angle one-way elastic wave equation [J].
Angus, D. A. .
GEOPHYSICS, 2007, 72 (02) :T19-T26
[7]   Numerical analysis of a narrow-angle, one-way, elastic-wave equation and extension to curvilinear coordinates [J].
Angus, D. A. ;
Thomson, C. J. .
GEOPHYSICS, 2006, 71 (05) :T137-T146
[8]   A one-way wave equation for modelling seismic waveform variations due to elastic heterogeneity [J].
Angus, DA .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2005, 162 (03) :882-898
[9]   A one-way wave equation for modelling variations in seismic waveforms due to elastic anisotropy [J].
Angus, DA ;
Thomson, CJ ;
Pratt, RG .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2004, 156 (03) :595-614
[10]   Modelling converted seismic waveforms in isotropic and anisotropic 1-D gradients: discontinuous versus continuous gradient representations [J].
Angus, Doug A. ;
Thomson, Colin J. .
STUDIA GEOPHYSICA ET GEODAETICA, 2012, 56 (02) :383-409