复杂介质地震波场研究进展
|
摘要
从传统的层状介质研究发展到对非均匀各向异性介质乃至随机介质研究,是解决当今高难度油气勘探和高标准油气开发问题的需要。面对这种发展趋势,近年来国内外有关学者进行了大量的复杂介质地震波场研究。本文对其在裂缝介质、双相介质及随机介质等方面的研究所取得的成果作一综述,以期为今后在该领域的研究积累较为系统的基础资料。
The development from traditional research of layered media to heterogeneous anisotropic media and to random media,is required to solve the problems in petroleum exploration.In resent years,a lot of researches of seismic required of complex medium have been done home and abroad.The authors reviewed the achievements of these researches of complex medium including fractured medium,bi-phase medium and random medium,so as to accumulate the basal systemic information for the future.
The development from traditional research of layered media to heterogeneous anisotropic media and to random media,is required to solve the problems in petroleum exploration.In resent years,a lot of researches of seismic required of complex medium have been done home and abroad.The authors reviewed the achievements of these researches of complex medium including fractured medium,bi-phase medium and random medium,so as to accumulate the basal systemic information for the future.
引文
[1]甘克文.国内外油气勘探前景解析[J].石油科技论坛,2004,5:21-25.GAN Ke-wen.Analysis of outlook of petroleum explo-ration at home and abroad[J].Oil Forum,2004,5:21-25.
[2]钱展.世界石油工程技术纵览[J].中国石油企业,2004,11:35-37.QIAN Zhan.Survey of technology of global petrolic engi-neering[J].Chinese Petroleum Enterprise,2004,11:35-37.
[3]何汉漪.二十一世纪的地震勘探技术[J].地学前缘,2000,3:267-273.HE Han-yi.The seismic technology in 21th century[J].Earth Science Frontiers,2000,3:267-273.
[4]王炳章.勘探地球物理方法技术的最新进展[J].石油地球物理勘探,1999,34(4):465-483.WANG Bing-Zhang.The lastest proceeding of geophysi-cal techniques[J].Oil Geophysical Prospecting,1999,34(4):465-483.
[5]Pritchett R W,Ray R R.A preview of the 11th annual 3Dseismic symposium“:Paths to Prosperity”[J].TheLeading Edge,2005,24(2):158.
[6]Hawkins K,Leggott R,Williams G,et al.Addressinganisotropy in 3-D prestack depth migration:a case studyfrom the southern North Sea[J].Leading Edge,2001,20(5):528.
[7]Carrion P M,Sampaio E E S.Imaging the earth-thequest for resolution[J].Leading Edge,1990,9(10):30-32.
[8]Yehuda B Z,Charls S,Tom H.Perspectives on the field ofphysics of earthquakes[J].Seismological Research Let-ters,1999,70(4):428.
[9]滕吉文,王光杰,杨顶辉,等.地球各向异性介质中地震波动理论、检测与应用研究[J].地学前缘,1998,5(1/2):83-90.TENG Ji-wen,WANG Guang-jie,YANG Ding-hui,et al.The study for propagation theory of seismic waves,detec-tion technique and application on anisotropic media in theearth's interior[J].Earth Science Frontiers,1998,5(1/2):83-90.
[10]张中杰.地震各向异性研究进展[J].地球物理学进展,2002,2:281-293.ZHANG Zhong-jie.A review of the seismic anisotropyand its applications[J].Progress in Geophysics,2002,2:281-293.
[11]滕吉文,张中杰.复杂地球介质中地震波动理论、检测技术与应用研究[J].科技导报,1995,4:43.TENG Ji-wen,ZHANG Zhong-jie.The study for propaga-tion theory of seismic waves,detection technique and ap-plication on complex media in the earth's interior[J].Science&Technology Review,1995,4:43.
[12]Hsu C J,Michael S.Elastic waves through a simulatedfractured medium[J].Geophysics,1993,58(7):964-977.
[13]Tariq AI,lya T.Velocity analysis for transversely isotrop-ic media[J].Geophysics,1995,60(5):1550-1566.
[14]HSN Q Y,WU R S.Depth imaging in strongly heteroge-neous VTI media[J].SEG Technical Program ExpandedAbstracts,2004,23:1061-1064.
[15]Patricia A B.Constraints on elastic parameters and impli-cations for lithology in VTI media[J].SEG TechnicalProgram Expanded Abstracts,1995,14:906-909.
[16]Ilya T.Reflection moveout and parameter estimation forhorizontal transverse isotropy[J].Geophysics,1997,62(2):614-629.
[17]Vladimir GI,lya T.Inversion of azimuthally dependentNMO velocity in transversely isotropic media with a tiltedaxis of symmetry[J].Geophysics,2000,65(1):232-246.
[18]Jaime R M,Andrey A O,George A M.3-D seismic mod-eling for cracked medias:hear-wave splitting at zero-off-set[J].Geophysics,2000,65(1):211-221.
[19]LOU M.Modeling study of marine multi-component seis-mic data in anisotropic fractured media by a Fourier me-thod[J].SEG Technical Program Expanded Abstracts,2000,19:2369-2372.
[20]Tobias M M.Green's function construction for 2D and 3Delastic random media[J].SEG Technical Program Ex-panded Abstracts,1999,18:1797-1800.
[21]Thomas B.Parallel finite-difference modeling of seismicwave scattering in 3-D elastic random media[J].SEGTechnical Program Expanded Abstracts,2001,20:1147-1150.
[22]Heloise B L.The winds of changea:nisotropic rocks-theirpreferred direction of fluid flow and their associated seis-mic signatures-part 1[J].Leading Edge,2004,23(11):1156-1162.
[23]Heloise B L.The winds of change:anisotropic rocks-their preferred direction of fluid flow and their associatedseismic signatures part 2[J].Leading Edge,2004,23(12):1258-1268.
[24]刘恩儒,曾新吾.裂缝介质的有效弹性常数[J].石油地球物理勘探,2001,36(1):37-44.LIU En-ru,ZENG Xin-wu.Effective elastic constant offractured medium[J].Oil Geophysical Prospecting,2001,36(1):37-44.
[25]张光莹,曾新吾.裂缝排列方向及界面对波的共同作用[J].石油地球物理勘探,2003,38(2):168-172.ZHANG Guang-ying,ZENG Xin-wu.Common action ofaligned fracture and interface on elastic wave[J].OilGeophysical Prospecting,2003,38(2):168-172.
[26]Grechka V,Bakulin A,Tsvankin I.Seismic characteriza-tion of vertical fractures described as general linear-slip in-terfaces[J].SEG Technical Program Expanded Abstr-acts,2001,20:2101-2104.
[27]Grechka V,Tsvankin I.Feasibility of seismic characteri-zation of multiple fracture sets[J].SEG Technical Pro-gram Expanded Abstracts,2002,21:1646-1649.
[28]Baren G B,Mulder W A,Herman G C.Finite-differencemodeling of scalar-wave propagation in cracked media[J].Geophysics,2001,66(1):267-276.
[29]杨顶辉,张中杰,滕吉文,等.双相各向异性研究、问题与应用前景[J].地球物理学进展,2000,15(2):7-21.YANG Ding-hui,ZHANG Zhong-jie,TENG Ji-wen,et al.The study of tow-phase anisotropy questions and appliedprospects[J].Progress in Geophysics,2000,15(2):7-21.
[30]Crampin S.The potential of shear-wave splittng in astress-sensitive compliant crusta:new understanding ofpre-fracturing deformation from time-lapse studies[J].SEG Technical Program Expanded Abstracts,2000,19:1520-1523.
[31]Daley P F.Conversion coefficients at a liquid/solid inter-face[J].SEG Technical Program Expanded Abstracts,2001,20:2065-2068.
[32]姚姚,奚先.区域多尺度随机介质模型及其波场分析[J].石油物探,2004,43(1):1-7.YAO Yao,XI Xian.Regionalized multi-scale randommedium model and its wavefield analysis[J].Geophysi-cal Prospecting for Petroleum,2004,43(1):1-7.
[33]Ikelle L T,Yung S K,Daube F.2-D random media withellipsoidal autocorrelation function[J].Geophysics,1993,58(9):1359-1372.
[34]Nizar C.Modeling 3-D anisotropic fractal media[J].Stanford Exploration Project,2001,80:1-13.
[35]Ergintav S,Canitez N.Modeling of multi-scale media indiscrete form[J].Journal of Seismic Exploration,1997,6:77-96.
[36]奚先,姚姚.随机介质模型的模拟与混合型随机介质[J].地球科学,2002,2(7 1):67-71.XI Xian,YAO Yao.Simulations of random medium mod-el and intermixed random medium[J].Earth Science,2002,2(7 1):67-71.
[37]Korn M.Seismic wave in random medi[a J].Journal ofApplied Geophys,1993,29:247-269.
[38]Roth M,Korn M.Single-scattering theory versus numeri-cal modeling in two-dimensional random med[ia J].Geo-physical Journal International,1993,112:124-140.
[39]Burridge R,Chang H W.Wave propagation in a highlydiscontinuous layered elastic medium[J].SEG TechnicalProgram Expanded Abstracts,1988,17:1350-1352.
[40]Sergei A S,Peter H.Elastic waves in finely layered sedi-ments:the equivalent medium and generalized O'Doher-ty-Anstey formula[s J].Geophysics,1996,6(1 5):1282-1300.
[41]Müller T M,Shapiro S A.Scattering attenuation in ran-domly layered structures with finite lateral extent:a hybridQ mod[el J].Geophysics,2004,6(9 6):1530-1534.
[42]杨宝俊,张伯军,杨有发,等.地震勘探频率中近抛物线型衰减的物理解释[J].长春地质学院学报,1990,20(3):323-330.YANG Bao-jun,ZHANG Bo-jun,YANG You-fa,et al.Physical interpretation of seismic wave's attenuation withnear parabola's model in seismic survey frequency's range[J].Journal of Changchun University of Earth Science,1990,2(0 3):323-330.
[43]Yoshimasa K.Delay of first arrival caused by dispersionof seismic body wave[s J].SEG Technical Program Ex-panded Abstracts,2001,20:2069-2072.
[44]Chesnokov E M,Vichorev A A,Bayuk I O,et al.Fre-quency dependent anisotropy[J].SEG Technical Pro-gram Expanded Abstracts,2001,20:2120-2123.
[45]Claudia K.Anisotropy in sedimentary rocks modeled asrandom med[ia J].Geophysics,1992,5(7 4):564-576.
[46]Guido K,Serge A S.Viscoacoustic wave propagation in2-D random media and separation of absorption and scat-tering attenuation[J].Geophysics,1995,6(0 2):459-467.
[47]奚先,姚姚.二维粘弹性随机介质中的波场特征分析[J].地球物理学进展,2004,1(9 3):608-615.XI Xian,YAO Yao.The analysis of the wave field charac-teristics in 2-D viscoelastic random medium[J].Progressin Geophysics,2004,1(9 3):608-615.
[2]钱展.世界石油工程技术纵览[J].中国石油企业,2004,11:35-37.QIAN Zhan.Survey of technology of global petrolic engi-neering[J].Chinese Petroleum Enterprise,2004,11:35-37.
[3]何汉漪.二十一世纪的地震勘探技术[J].地学前缘,2000,3:267-273.HE Han-yi.The seismic technology in 21th century[J].Earth Science Frontiers,2000,3:267-273.
[4]王炳章.勘探地球物理方法技术的最新进展[J].石油地球物理勘探,1999,34(4):465-483.WANG Bing-Zhang.The lastest proceeding of geophysi-cal techniques[J].Oil Geophysical Prospecting,1999,34(4):465-483.
[5]Pritchett R W,Ray R R.A preview of the 11th annual 3Dseismic symposium“:Paths to Prosperity”[J].TheLeading Edge,2005,24(2):158.
[6]Hawkins K,Leggott R,Williams G,et al.Addressinganisotropy in 3-D prestack depth migration:a case studyfrom the southern North Sea[J].Leading Edge,2001,20(5):528.
[7]Carrion P M,Sampaio E E S.Imaging the earth-thequest for resolution[J].Leading Edge,1990,9(10):30-32.
[8]Yehuda B Z,Charls S,Tom H.Perspectives on the field ofphysics of earthquakes[J].Seismological Research Let-ters,1999,70(4):428.
[9]滕吉文,王光杰,杨顶辉,等.地球各向异性介质中地震波动理论、检测与应用研究[J].地学前缘,1998,5(1/2):83-90.TENG Ji-wen,WANG Guang-jie,YANG Ding-hui,et al.The study for propagation theory of seismic waves,detec-tion technique and application on anisotropic media in theearth's interior[J].Earth Science Frontiers,1998,5(1/2):83-90.
[10]张中杰.地震各向异性研究进展[J].地球物理学进展,2002,2:281-293.ZHANG Zhong-jie.A review of the seismic anisotropyand its applications[J].Progress in Geophysics,2002,2:281-293.
[11]滕吉文,张中杰.复杂地球介质中地震波动理论、检测技术与应用研究[J].科技导报,1995,4:43.TENG Ji-wen,ZHANG Zhong-jie.The study for propaga-tion theory of seismic waves,detection technique and ap-plication on complex media in the earth's interior[J].Science&Technology Review,1995,4:43.
[12]Hsu C J,Michael S.Elastic waves through a simulatedfractured medium[J].Geophysics,1993,58(7):964-977.
[13]Tariq AI,lya T.Velocity analysis for transversely isotrop-ic media[J].Geophysics,1995,60(5):1550-1566.
[14]HSN Q Y,WU R S.Depth imaging in strongly heteroge-neous VTI media[J].SEG Technical Program ExpandedAbstracts,2004,23:1061-1064.
[15]Patricia A B.Constraints on elastic parameters and impli-cations for lithology in VTI media[J].SEG TechnicalProgram Expanded Abstracts,1995,14:906-909.
[16]Ilya T.Reflection moveout and parameter estimation forhorizontal transverse isotropy[J].Geophysics,1997,62(2):614-629.
[17]Vladimir GI,lya T.Inversion of azimuthally dependentNMO velocity in transversely isotropic media with a tiltedaxis of symmetry[J].Geophysics,2000,65(1):232-246.
[18]Jaime R M,Andrey A O,George A M.3-D seismic mod-eling for cracked medias:hear-wave splitting at zero-off-set[J].Geophysics,2000,65(1):211-221.
[19]LOU M.Modeling study of marine multi-component seis-mic data in anisotropic fractured media by a Fourier me-thod[J].SEG Technical Program Expanded Abstracts,2000,19:2369-2372.
[20]Tobias M M.Green's function construction for 2D and 3Delastic random media[J].SEG Technical Program Ex-panded Abstracts,1999,18:1797-1800.
[21]Thomas B.Parallel finite-difference modeling of seismicwave scattering in 3-D elastic random media[J].SEGTechnical Program Expanded Abstracts,2001,20:1147-1150.
[22]Heloise B L.The winds of changea:nisotropic rocks-theirpreferred direction of fluid flow and their associated seis-mic signatures-part 1[J].Leading Edge,2004,23(11):1156-1162.
[23]Heloise B L.The winds of change:anisotropic rocks-their preferred direction of fluid flow and their associatedseismic signatures part 2[J].Leading Edge,2004,23(12):1258-1268.
[24]刘恩儒,曾新吾.裂缝介质的有效弹性常数[J].石油地球物理勘探,2001,36(1):37-44.LIU En-ru,ZENG Xin-wu.Effective elastic constant offractured medium[J].Oil Geophysical Prospecting,2001,36(1):37-44.
[25]张光莹,曾新吾.裂缝排列方向及界面对波的共同作用[J].石油地球物理勘探,2003,38(2):168-172.ZHANG Guang-ying,ZENG Xin-wu.Common action ofaligned fracture and interface on elastic wave[J].OilGeophysical Prospecting,2003,38(2):168-172.
[26]Grechka V,Bakulin A,Tsvankin I.Seismic characteriza-tion of vertical fractures described as general linear-slip in-terfaces[J].SEG Technical Program Expanded Abstr-acts,2001,20:2101-2104.
[27]Grechka V,Tsvankin I.Feasibility of seismic characteri-zation of multiple fracture sets[J].SEG Technical Pro-gram Expanded Abstracts,2002,21:1646-1649.
[28]Baren G B,Mulder W A,Herman G C.Finite-differencemodeling of scalar-wave propagation in cracked media[J].Geophysics,2001,66(1):267-276.
[29]杨顶辉,张中杰,滕吉文,等.双相各向异性研究、问题与应用前景[J].地球物理学进展,2000,15(2):7-21.YANG Ding-hui,ZHANG Zhong-jie,TENG Ji-wen,et al.The study of tow-phase anisotropy questions and appliedprospects[J].Progress in Geophysics,2000,15(2):7-21.
[30]Crampin S.The potential of shear-wave splittng in astress-sensitive compliant crusta:new understanding ofpre-fracturing deformation from time-lapse studies[J].SEG Technical Program Expanded Abstracts,2000,19:1520-1523.
[31]Daley P F.Conversion coefficients at a liquid/solid inter-face[J].SEG Technical Program Expanded Abstracts,2001,20:2065-2068.
[32]姚姚,奚先.区域多尺度随机介质模型及其波场分析[J].石油物探,2004,43(1):1-7.YAO Yao,XI Xian.Regionalized multi-scale randommedium model and its wavefield analysis[J].Geophysi-cal Prospecting for Petroleum,2004,43(1):1-7.
[33]Ikelle L T,Yung S K,Daube F.2-D random media withellipsoidal autocorrelation function[J].Geophysics,1993,58(9):1359-1372.
[34]Nizar C.Modeling 3-D anisotropic fractal media[J].Stanford Exploration Project,2001,80:1-13.
[35]Ergintav S,Canitez N.Modeling of multi-scale media indiscrete form[J].Journal of Seismic Exploration,1997,6:77-96.
[36]奚先,姚姚.随机介质模型的模拟与混合型随机介质[J].地球科学,2002,2(7 1):67-71.XI Xian,YAO Yao.Simulations of random medium mod-el and intermixed random medium[J].Earth Science,2002,2(7 1):67-71.
[37]Korn M.Seismic wave in random medi[a J].Journal ofApplied Geophys,1993,29:247-269.
[38]Roth M,Korn M.Single-scattering theory versus numeri-cal modeling in two-dimensional random med[ia J].Geo-physical Journal International,1993,112:124-140.
[39]Burridge R,Chang H W.Wave propagation in a highlydiscontinuous layered elastic medium[J].SEG TechnicalProgram Expanded Abstracts,1988,17:1350-1352.
[40]Sergei A S,Peter H.Elastic waves in finely layered sedi-ments:the equivalent medium and generalized O'Doher-ty-Anstey formula[s J].Geophysics,1996,6(1 5):1282-1300.
[41]Müller T M,Shapiro S A.Scattering attenuation in ran-domly layered structures with finite lateral extent:a hybridQ mod[el J].Geophysics,2004,6(9 6):1530-1534.
[42]杨宝俊,张伯军,杨有发,等.地震勘探频率中近抛物线型衰减的物理解释[J].长春地质学院学报,1990,20(3):323-330.YANG Bao-jun,ZHANG Bo-jun,YANG You-fa,et al.Physical interpretation of seismic wave's attenuation withnear parabola's model in seismic survey frequency's range[J].Journal of Changchun University of Earth Science,1990,2(0 3):323-330.
[43]Yoshimasa K.Delay of first arrival caused by dispersionof seismic body wave[s J].SEG Technical Program Ex-panded Abstracts,2001,20:2069-2072.
[44]Chesnokov E M,Vichorev A A,Bayuk I O,et al.Fre-quency dependent anisotropy[J].SEG Technical Pro-gram Expanded Abstracts,2001,20:2120-2123.
[45]Claudia K.Anisotropy in sedimentary rocks modeled asrandom med[ia J].Geophysics,1992,5(7 4):564-576.
[46]Guido K,Serge A S.Viscoacoustic wave propagation in2-D random media and separation of absorption and scat-tering attenuation[J].Geophysics,1995,6(0 2):459-467.
[47]奚先,姚姚.二维粘弹性随机介质中的波场特征分析[J].地球物理学进展,2004,1(9 3):608-615.XI Xian,YAO Yao.The analysis of the wave field charac-teristics in 2-D viscoelastic random medium[J].Progressin Geophysics,2004,1(9 3):608-615.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心