MODELING GUIDED-WAVES IN CROSS-HOLE SURVEYS IN UNCRACKED AND CRACKED ROCK

被引:1
作者
LOU, M [1 ]
CRAMPIN, S [1 ]
机构
[1] UNIV EDINBURGH,DEPT GEOL & GEOPHYS,EDINBURGH EH9 3JZ,MIDLOTHIAN,SCOTLAND
关键词
D O I
10.1111/j.1365-2478.1993.tb00569.x
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 theoretical behaviour of guided waves in cross-hole seismic surveys is examined with dispersion curves and synthetic seismograms. The modelling suggests, and field observations confirm, that the dominant energy in many cross-hole seismic surveys propagates as guided waves, as well as body waves, with the energy tied to an interface, or combination of interfaces, whenever there are interfaces with significant velocity contrasts continuous between the wells. The dispersion and waveforms of such modal solutions carry detailed information about the internal structure, particularly the stress-aligned structure of fluid-filled inclusions in the immediate neighbourhood of the waveguide. Since the information content can be controlled to some extent by the choice of frequency and source type and the level of source and receiver in the two wells, such guided waves in cross-hole surveys may be important for monitoring changes in nearly horizontal reservoirs during hydrocarbon production processes. Initially, we investigate the basic properties of propagation in isotropic strata, and then examine the behaviour of guided waves in the stress-aligned fluid-filled inclusions.
引用
收藏
页码:241 / 265
页数:25
相关论文
共 29 条
[1]   DISPERSION CALCULATIONS FOR SH AND P-SV WAVES IN MULTILAYERED COAL SEAMS [J].
BUCHANAN, DJ .
GEOPHYSICAL PROSPECTING, 1987, 35 (01) :62-70
[2]   A DECADE OF SHEAR-WAVE SPLITTING IN THE EARTHS CRUST - WHAT DOES IT MEAN - WHAT USE CAN WE MAKE OF IT - AND WHAT SHOULD WE DO NEXT [J].
CRAMPIN, S ;
LOVELL, JH .
GEOPHYSICAL JOURNAL INTERNATIONAL, 1991, 107 (03) :387-407
[3]   DISTINCTIVE PARTICLE MOTION OF SURFACE-WAVES AS A DIAGNOSTIC OF ANISOTROPIC LAYERING [J].
CRAMPIN, S .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1975, 40 (02) :177-186
[4]   GEOLOGICAL AND INDUSTRIAL IMPLICATIONS OF EXTENSIVE-DILATANCY ANISOTROPY [J].
CRAMPIN, S .
NATURE, 1987, 328 (6130) :491-496
[5]   EARTHQUAKE PREDICTION - A NEW PHYSICAL BASIS [J].
CRAMPIN, S ;
EVANS, R ;
ATKINSON, BK .
GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1984, 76 (01) :147-156
[6]   SUGGESTIONS FOR A CONSISTENT TERMINOLOGY FOR SEISMIC ANISOTROPY [J].
CRAMPIN, S .
GEOPHYSICAL PROSPECTING, 1989, 37 (07) :753-770
[7]  
Crampin S., 1984, 1 BREAK, V2, P19, DOI DOI 10.3997/1365-2397.1984006
[8]  
Crampin S., 1985, FIRST BREAK, V3, P12, DOI [10.3997/1365-2397.1985004, DOI 10.3997/1365-2397.1985004]
[9]   THE INFLUENCE OF AN ASYMMETRY IN THE SEQUENCE ROCK COAL ROCK ON THE PROPAGATION OF RAYLEIGH SEAM WAVES [J].
DRESEN, L ;
KERNER, C ;
KUHBACH, B .
GEOPHYSICAL PROSPECTING, 1985, 33 (04) :519-539
[10]   OVERALL PROPERTIES OF A CRACKED SOLID [J].
HUDSON, JA .
MATHEMATICAL PROCEEDINGS OF THE CAMBRIDGE PHILOSOPHICAL SOCIETY, 1980, 88 (SEP) :371-384