国内外深反射地震研究的进展及应用研究
|
摘要
当前探测深部构造的地球物理技术主要是地震学的方法,其中的深反射地震技术目前被国际地学界公认为探测岩石圈精细结构的高技术。美国于20世纪70年代中期首先利用该技术来研究地壳结构深部构造的问题,并取得了很好的研究结果。随后英、法、德、加拿大和澳大利亚等国家相继开展了深地震反射研究计划,获得了岩石圈的形成与演化、地球深部构造等方面的重要信息。我国从20世纪80年代开始利用深地震反射技术来研究造山带形成机制和演化模式,研究结果对地震的孕育和发生的深部环境以及地学上的重大问题取得了突破性的认识。
Currently seismological methods are the primary methods in deep structure exploration. International geologists have recognized deep seismic reflection as high technology in probing fine structure of lithosphere. In the 1970s, the technology had been applied to crustal structure and deep structure study with good result in USA. Subsequently Britain, France, Germany, Canada, Australia developed deep seismic reflection research, and obtained lots of important information about form, development and deep structure. In the 1980s, China began to apply deep seismic reflection to the research of formation mechanism and evolution mode of orogenic belt and the results broke through the normal recognition about earthquake, deep circumstance and some important questions in geology.
Currently seismological methods are the primary methods in deep structure exploration. International geologists have recognized deep seismic reflection as high technology in probing fine structure of lithosphere. In the 1970s, the technology had been applied to crustal structure and deep structure study with good result in USA. Subsequently Britain, France, Germany, Canada, Australia developed deep seismic reflection research, and obtained lots of important information about form, development and deep structure. In the 1980s, China began to apply deep seismic reflection to the research of formation mechanism and evolution mode of orogenic belt and the results broke through the normal recognition about earthquake, deep circumstance and some important questions in geology.
引文
[1]Brown L,Barazangi M,Kaufman S,Olicer J.The first decade of CO-CORP:1974～1984[A].In:eds.Barazangi,M.and Brown L.D.Re-flection seismology:A global perspective[C].American Geophysical Union Geodynamics Series,V.,1986,13:107～120
[2]Oliver J.COCORP probes continental depths[J].Geotimes,1993(june):21～22
[3]Clowes R M.LITHOPROBE:An integrated approach to studie s of crustal evolution[J].Geotimes,1992,(Agu):12～14
[4]Brun J P,Gustcher M A.DEKORP-ECORS teama,Deep crustal structure of the Rhine Groben from DECORP-ECORS seismic re-flection data:a summary[J].Tectonophysics,208:139～147
[5]Matthews D H,The BIRPS Group.Progress in BIRPS deep seismic reflection profiling around the British Isles[J].Tectonophysics.1990,173:387～396
[6]Bois C.ECORS Scientific Party.Major geodynamic processes studies from the ECORS deep seismic profiles in France and adjacent ar-eas[J].Tectonophysics.1990,173:397～410
[7]Moss F J,Mathur S P.A review of continental reflection profiling in Australia[A].In:eds.Barazangi,M.and Brown L.D.Reflection seis-mology:A global perspective[C].American Geophysical Union Geo-dynamics Series,V.1986,13:67～76
[8]梁慧云,张先康.各国地壳上地幔深地震反射研究计划与进展[J].地球物理学进展,1996,11(1):42～60
[9]黄立言,高锐.深地震反射剖面数据子库[J].地球学报,2001,22(6):491～496
[10]赵文津,KDNelson,纳尔逊.印度板块俯冲到藏南之下的深反射证据[J].地球学报,1996,17(2):131～137
[11]赵文津,Nelson KD,Brown LD,等.喜马拉雅和西藏高原深地震反射剖面(INDEPTH)概况[R].地球物理学报,36,125
[12]赵文津,Nelson KD,高锐,等.喜马拉雅和西藏高原深地震反射剖面的初步成果[J].地球物理学报,36,125
[13]傅维洲,杨宝俊,刘财.中国满洲里—绥芬河地学断面地震学研究[J].长春科技大学学报,1998,28(2):206～212
[14]高锐,吴功建.青藏高原亚东—格尔木地学断面地球物理综合解释模型与现今地球物理动力学过程[J].长春地质学院学报,1995,25(3):241～250
[15]曾融生,陆涵行,丁志峰.从地震折射和反射剖面结果讨论唐山地震成因[J].地球物理学报,1988,31:383～398
[16]吴宣志,吴春玲.利用深地震反射剖面研究北祁连—河西走廊地壳细结构[J].地球物理学报,1995,38(增刊II):29～35
[17]高锐,黄东定,卢德源,等.横过西昆仑—塔里木接触带德深反射地震剖面[J].科学通报,2000,45(17):1874～1879
[18]高锐,肖序常,刘训,等.新疆地学断面深地震反射剖面揭示德西昆仑—塔里木结合带岩石圈细结构[J].地球学报,2001,22(6):547～569
[19]高锐,董树文,贺日政,等.莫霍面地震反射图像揭露出扬子陆块深俯冲过程[J].地学前缘,2004,11(3):43～49
[20]高锐,李秋生.燕山造山带深地震反射剖面启动探测研究[J].地质通报,2002,21(12):905～906
[21]ZHAO W,NELSON D.Project INDEPTH team.Deep seismic re-flection evidence for continental underthrusting beneath southern Tibet[J].Nature,1993,366:557～559
[22]GAO Rui,HUANG Dong-ding,L U Deyuan,et al.Deep seismic re-flection profiles across contact zone of West Kunlun and Tarim basin along the Xinjiang geotransect in NW Chin[J].Terra Nostra,1999,2(99):49～50
[23]GAO Rui,HUANG Dong-ding,LU Deyuan,et al.Deep seismic re-flection profiles across juncture zone between Tarim basin and west Kunlun Mountain[J].Chinese Science Bulletin,2000,45(17):1874～1849
[24]YUAN X C,KLEMPERPER S L,TENG W B,et al.Crustal structure and exhumation of the Dabie Shan ultrahigh-pressure orogen,east-ern China,from seismic reflection profiling[A].Proceedings for In-ternational UHPM Workshop[C].Beijing:2002,13
[25]YUAN X C,KLEMPERPER S L,TENG W B,et al.Crustal structure and exhumation of the Dabie Shan ultrahigh-pressure orogen,east-ern China,from seismic reflection profiling[J].Geology,2003,31:435～438
[26]Dewey J,Kempton M,Kidd W,et al.Shortening of continental lithosphere:the neotectonics of Eastern Analolia-a young colli-sion zone,In:Collision tectonics,eds.M.Coward and A.Ries,1986:3～36
[27]Bois C.Geological significance of seismic reflections in collision belts[J].Geophys.J.Int.,1991,105:55～69
[28]Meissner R,Wever Th,Sadowiak P.Continental collisions and seis-mic signature[J].Geophy.J.Int,1991,105:15～23
[29]Meissner R.Rupture creep,lamellae and crocodiles happenings in the continental crust[J].Tera nova,1989,1:17～28
[30]吴福元,张世红.深反射地震调查对大地构造学的贡献[J].世界地质,1994,13(1):117～127
[31]Cheadle M J,Czuchra B L,Ando C J,et al.Geometries of deep crustal faults:evidence from the COCORP Mojave survey[A].In:Reflection seismology:the continental crust[C].eds.M.Barazangi and L.D.Brown,Am.Geophys.Uinon,Geodyn,Ser.,1986,14:305～312
[32]Feng R.,McErilly T V.Interpretation of seismic reflection profiling data for the structure of the San Andreas Fault zone[A].Bull.Seis.Soc.Am,1983,73:1701～1720
[33]Meissner R,Wever Th.Nature and development of the crust ac-cording to deep reflection data from the German Variscides[A].In:Reflection seismology:A Global perspective[C].eds.M.Barazangi and L.D.Brown.Geodyn.Ser.,1986,13:31￣42
[34]Hale L D,Thompson S A.The seismic reflection character of the continental Mohorovicic discontinuity.J.Geophys.Res.1982,87:4625～4635
[35]Allmendinger R W,Nelson K D,Potter C J,et al.Deep seismic re-flection characteristics of the continental crust[J].Geology,1987,15:304～310
[36]Nelson K D.A Unfied view of craton evolution motivated by recent deep seismic reflection and refraction results[J].Geophy.J.Int.,1991,105:25～35
[37]BROWN L D,WILLE D M,ZHENG L,et al.COCORP:Newperspec-tives on the deep crust[J].Geophys J R AstrSoc,1987,89:47～54
[38]HAMMER P T C,CLOWES R T.Moho reflectivity patterns-A com-parison of Canadian LITHOPROBE Transects[J].Tectonophysics,1997,269:179～198
[39]彭聪,赵一鸣.中国东部含金矽卡岩矿床分布规律与深部地球物理背景研究[J].物探与化探,1999,23(6):415～420
[40]吕庆田等.深地震反射剖面揭示的铜陵矿集区复杂地壳结构形态[J].中国科学,2003,33(5):442～449
[2]Oliver J.COCORP probes continental depths[J].Geotimes,1993(june):21～22
[3]Clowes R M.LITHOPROBE:An integrated approach to studie s of crustal evolution[J].Geotimes,1992,(Agu):12～14
[4]Brun J P,Gustcher M A.DEKORP-ECORS teama,Deep crustal structure of the Rhine Groben from DECORP-ECORS seismic re-flection data:a summary[J].Tectonophysics,208:139～147
[5]Matthews D H,The BIRPS Group.Progress in BIRPS deep seismic reflection profiling around the British Isles[J].Tectonophysics.1990,173:387～396
[6]Bois C.ECORS Scientific Party.Major geodynamic processes studies from the ECORS deep seismic profiles in France and adjacent ar-eas[J].Tectonophysics.1990,173:397～410
[7]Moss F J,Mathur S P.A review of continental reflection profiling in Australia[A].In:eds.Barazangi,M.and Brown L.D.Reflection seis-mology:A global perspective[C].American Geophysical Union Geo-dynamics Series,V.1986,13:67～76
[8]梁慧云,张先康.各国地壳上地幔深地震反射研究计划与进展[J].地球物理学进展,1996,11(1):42～60
[9]黄立言,高锐.深地震反射剖面数据子库[J].地球学报,2001,22(6):491～496
[10]赵文津,KDNelson,纳尔逊.印度板块俯冲到藏南之下的深反射证据[J].地球学报,1996,17(2):131～137
[11]赵文津,Nelson KD,Brown LD,等.喜马拉雅和西藏高原深地震反射剖面(INDEPTH)概况[R].地球物理学报,36,125
[12]赵文津,Nelson KD,高锐,等.喜马拉雅和西藏高原深地震反射剖面的初步成果[J].地球物理学报,36,125
[13]傅维洲,杨宝俊,刘财.中国满洲里—绥芬河地学断面地震学研究[J].长春科技大学学报,1998,28(2):206～212
[14]高锐,吴功建.青藏高原亚东—格尔木地学断面地球物理综合解释模型与现今地球物理动力学过程[J].长春地质学院学报,1995,25(3):241～250
[15]曾融生,陆涵行,丁志峰.从地震折射和反射剖面结果讨论唐山地震成因[J].地球物理学报,1988,31:383～398
[16]吴宣志,吴春玲.利用深地震反射剖面研究北祁连—河西走廊地壳细结构[J].地球物理学报,1995,38(增刊II):29～35
[17]高锐,黄东定,卢德源,等.横过西昆仑—塔里木接触带德深反射地震剖面[J].科学通报,2000,45(17):1874～1879
[18]高锐,肖序常,刘训,等.新疆地学断面深地震反射剖面揭示德西昆仑—塔里木结合带岩石圈细结构[J].地球学报,2001,22(6):547～569
[19]高锐,董树文,贺日政,等.莫霍面地震反射图像揭露出扬子陆块深俯冲过程[J].地学前缘,2004,11(3):43～49
[20]高锐,李秋生.燕山造山带深地震反射剖面启动探测研究[J].地质通报,2002,21(12):905～906
[21]ZHAO W,NELSON D.Project INDEPTH team.Deep seismic re-flection evidence for continental underthrusting beneath southern Tibet[J].Nature,1993,366:557～559
[22]GAO Rui,HUANG Dong-ding,L U Deyuan,et al.Deep seismic re-flection profiles across contact zone of West Kunlun and Tarim basin along the Xinjiang geotransect in NW Chin[J].Terra Nostra,1999,2(99):49～50
[23]GAO Rui,HUANG Dong-ding,LU Deyuan,et al.Deep seismic re-flection profiles across juncture zone between Tarim basin and west Kunlun Mountain[J].Chinese Science Bulletin,2000,45(17):1874～1849
[24]YUAN X C,KLEMPERPER S L,TENG W B,et al.Crustal structure and exhumation of the Dabie Shan ultrahigh-pressure orogen,east-ern China,from seismic reflection profiling[A].Proceedings for In-ternational UHPM Workshop[C].Beijing:2002,13
[25]YUAN X C,KLEMPERPER S L,TENG W B,et al.Crustal structure and exhumation of the Dabie Shan ultrahigh-pressure orogen,east-ern China,from seismic reflection profiling[J].Geology,2003,31:435～438
[26]Dewey J,Kempton M,Kidd W,et al.Shortening of continental lithosphere:the neotectonics of Eastern Analolia-a young colli-sion zone,In:Collision tectonics,eds.M.Coward and A.Ries,1986:3～36
[27]Bois C.Geological significance of seismic reflections in collision belts[J].Geophys.J.Int.,1991,105:55～69
[28]Meissner R,Wever Th,Sadowiak P.Continental collisions and seis-mic signature[J].Geophy.J.Int,1991,105:15～23
[29]Meissner R.Rupture creep,lamellae and crocodiles happenings in the continental crust[J].Tera nova,1989,1:17～28
[30]吴福元,张世红.深反射地震调查对大地构造学的贡献[J].世界地质,1994,13(1):117～127
[31]Cheadle M J,Czuchra B L,Ando C J,et al.Geometries of deep crustal faults:evidence from the COCORP Mojave survey[A].In:Reflection seismology:the continental crust[C].eds.M.Barazangi and L.D.Brown,Am.Geophys.Uinon,Geodyn,Ser.,1986,14:305～312
[32]Feng R.,McErilly T V.Interpretation of seismic reflection profiling data for the structure of the San Andreas Fault zone[A].Bull.Seis.Soc.Am,1983,73:1701～1720
[33]Meissner R,Wever Th.Nature and development of the crust ac-cording to deep reflection data from the German Variscides[A].In:Reflection seismology:A Global perspective[C].eds.M.Barazangi and L.D.Brown.Geodyn.Ser.,1986,13:31￣42
[34]Hale L D,Thompson S A.The seismic reflection character of the continental Mohorovicic discontinuity.J.Geophys.Res.1982,87:4625～4635
[35]Allmendinger R W,Nelson K D,Potter C J,et al.Deep seismic re-flection characteristics of the continental crust[J].Geology,1987,15:304～310
[36]Nelson K D.A Unfied view of craton evolution motivated by recent deep seismic reflection and refraction results[J].Geophy.J.Int.,1991,105:25～35
[37]BROWN L D,WILLE D M,ZHENG L,et al.COCORP:Newperspec-tives on the deep crust[J].Geophys J R AstrSoc,1987,89:47～54
[38]HAMMER P T C,CLOWES R T.Moho reflectivity patterns-A com-parison of Canadian LITHOPROBE Transects[J].Tectonophysics,1997,269:179～198
[39]彭聪,赵一鸣.中国东部含金矽卡岩矿床分布规律与深部地球物理背景研究[J].物探与化探,1999,23(6):415～420
[40]吕庆田等.深地震反射剖面揭示的铜陵矿集区复杂地壳结构形态[J].中国科学,2003,33(5):442～449
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