深地震反射剖面揭露大陆岩石圈精细结构
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
深地震反射技术已被国际地学界公认为是探测岩石圈精细结构、解决深部地质问题的有效技术手段。自上世纪70年代中期以来,以美国为首的等西方国家和中国相继开展了深地震反射探测技术实验,使用该技术揭露盆地、造山带岩石圈的形成和演化、地球动力学过程,并应用于油气资源远景评价、矿产资源勘察等领域,取得了丰硕的成果。本文扼要介绍深地震反射剖面技术的发展及其部分应用实例。
Deep seismic reflection has currently been recognized as an effective technological approach in probing fine structure of lithosphere and solving the deep geological problems. Since the 1970s, the western countries with America as a leading one and China have successively carried out deep seismic reflection exploration program. The technology of this kind has been widely used to disclose the formation and evolution of lithosphere in basins and the orogenic belts, geodynamics processes, and has been applied in prospective evaluation of oil and gas resources, mineral resources exploration and other fields. A large amount of results have been achieved. The development of deep seismic reflection technique and its part of the applications example are described briefly in this paper.
引文
柴炽章,孟广魁,杜鹏,王银等.2006.隐伏活动断层的多层次综合探测—以银川隐伏活动断层为例.地震地质,28(4):536~546.
    陈沪生,周雪涛.1988.下杨子地区HQ-13浅地球物理-地质综合解释剖面.地质论评,34(6):483~484.
    董树文,高锐,李秋生,刘晓春,等.2005.大别山造山带前陆深地震反射剖面.地质学报,79(5):595~601.
    董树文,李廷栋.2009.SinoProbe——中国深部探测实验.地质学报,83(7):895~909.
    樊计昌,李松林,张先康,等.2004.海原断裂在地壳深处的几何形态及其动力学意义.地震学报,26(增刊):42~49.
    高锐,黄东定,卢德源,等.2000.横过西昆仑-塔里木结合带的深地震反射剖面.科学通报,45(17):1874~1879.
    高锐,李朋武,李秋生,管烨,史大年,等.2001a.青藏高原北缘碰撞变形的深部过程.中国科学(D辑),31(增刊):66~71.
    高锐,肖序常,刘训,管烨,李秋生,卢德源,李朋武.2001b.新疆地学断面深地震反射剖面揭示的西昆仑-塔里木结合带岩石圈细结构.地球学报,22(6):547~552.
    高锐,肖序常,高弘,李秋生,刘训,姜枚,史大年,管烨.2002a.西昆仑—塔里木—天山岩石圈深地震探测.地质通报,21(1):11~18.
    高锐,李秋生,赵越,张季生,管烨,白金,等.2002b.燕山造山带深地震反射剖面启动探测研究.地质通报,21(12):905~906.
    高锐,董树文,贺日政,刘晓春,钱桂华,等.2004莫霍面地震反射图像揭露出扬子陆块俯冲过程,地学前缘,11(3):43~49.
    高锐,王海燕,马永生,朱铉,李秋生,李朋武,匡朝阳,卢占武.2006a.松潘地块若尔盖盆地与西秦岭造山带岩石圈尺度的构造关系——深地震反射剖面探测成果.地球学报,27(5):411~418.
    高锐,马永生,李秋生,朱铉,等.2006b.松潘地块与西秦岭造山带下地壳的性质与关系——深地震反射剖面的揭露.地质通报,25(12):1361~1367.
    黄春菊,周蒂,陈长民,等.2005.深反射地震剖面所揭示的白云凹陷的深部地壳结构.科学通报,50(10):1024~1031.
    侯贺晟,高锐,卢占武.2009.青藏高原羌塘中央隆起近地表速度结构的初至波层析成像试验.地质通报,28(6):738~745.
    侯贺晟,高锐,贺日政,刘金凯,酆少英,管烨,James Knapp,FrancisWu.2010.盆山结合部近地表速度结构与静校正方法研究——以西南天山与塔里木盆地结合带为例.石油物探,49:7~11.
    梁慧云.1990.法国ECORS的主要科学成果及展望.国际地震动态,9:26~28.
    梁慧云,张先康.1996.各国地壳上地幔深地震反射研究计划与进展.地球物理学进展,11(1):42~60.
    梁慧云,张先康.2004.俄罗斯的人工地震探测研究进展.大地测量与地球动力学,24(4):117~122.
    刘保金,沈军,张先康,等.2007.深地震反射剖面揭示的天山北缘乌鲁木齐坳陷地壳结构和构造.地球物理学报,50(5):1464~1472.
    刘保金,柴炽章,酆少英,等.2008.第四纪沉积区断层及其上断点探测的地震方法技术——以银川隐伏活动断层为例.地球物理学报,51(5):1475~1483.
    刘和甫,李晓清,刘立群,等.2004.走滑构造体系盆山耦合与区带分析.现代地质,18(2):139~150.
    陆涵行,曾融生,郭建明,林中洋.1988.唐山震区深反射剖面分析.地球物理学报,31:27~36.
    卢占武,高锐,李秋生,匡朝阳,刘金凯,等.2009a.藏北羌塘盆地反射地震剖面与叠加速度研究.中国地质,6:677~681。
    卢占武,高锐,李秋生,等.2009b.横过青藏高原羌塘地体中央隆起区的深反射地震试验剖面.地球物理学报,8:2008~2014.
    李勤学.2000.松辽盆地(北)范围内莫霍特征研究——用近垂直地震反射资料.(原)长春科技大学地球物理系博士研究生学位论文.
    吕庆田,侯增谦,赵金花,等.2003.深地震反射剖面揭示的铜陵矿集区复杂地壳结构形态.中国科学(D辑),33(5):442~449.
    吕庆田,侯增谦,史大年,等.2004a.铜陵狮子山金属矿地震反射结果及对区域找矿的意义.矿床地质,23(4):390~398.
    吕庆田,侯增谦,杨竹森,等.2004b.长江中下游地区的底侵作用及动力学演化模式:来自地球物理资料的约束.中国科学(D辑),34(9):783~794.
    师亚芹,冯希杰,戴王强,李晓妮,任隽,种瑾.2008.临潼—长安断裂带的几何结构及形成机理.地震学报,30(2):1522~2164.
    滕吉文,等.1974.柴达木东盆地的深层地震反射波和地壳结构.地球物理学报,17(2):122~134.
    滕吉文.2005.参加2004年第32届国际地质大会的点滴见闻与思考.地球物理学进展,20(3):577~583.
    王椿镛,王贵美,林中洋,等.1993.用深地震反射方法研究邢台地震区地壳细结构.地球物理学报,36:410~415.
    王椿镛,张先康,吴庆举.1994a.冀中坳陷内深地震反射剖面揭示的滑脱构造.科学通报:25~628.
    王椿镛,张先康,吴庆举,等.1994b.华北盆地滑脱构造的地震学证据.地球物理学报,37:613~620.
    王椿镛,张先康,林中洋,等.1994c.束鹿断陷盆地及其邻近的地壳结构特征.地震学报,16(4):472~479.
    王椿镛,楼海,魏修成,等.2001.天山北缘的地壳结构和1906年玛纳斯地震的地震构造.地震学报,23(5):460~470.
    王海燕,高锐,卢占武,等.2006.地球深部探测的先锋——深地震反射方法的发展与应用.勘探地球物理进展,29(1):7~13.
    王海燕,高锐,马永生,朱铉,李秋生,等.2007a.青藏高原东北缘盆山结合部位深地震反射资料处理方法与初步地质认识.中国地质,34(1):142~148.
    王海燕,高锐,马永生,等.2007b.若尔盖与西秦岭地震反射岩石圈结构和盆山耦合.地球物理学报,50(2):472~481.
    吴宣志,吴春玲,卢杰,等.1995.利用深地震反射剖面研究北祁连—河西走廊地壳细结构.地球物理学报,38(增刊II):29~35.
    徐树桐,袁学诚,吴维平,刘贻灿.2008.大别山黄石-六安反射地震剖面新的地质解释.地质通报,27(1):19~26.
    徐志琴,曾令森,杨经绥,等.2004.走滑断裂、“挤压性盆-山构造”与油气资源关系的探讨.地球科学-中国地质大学学报,29(6):631~643.
    熊小松,高锐,李秋生,卢占武.2009.深地震探测揭示的华南地区莫霍面深度,地球学报,30(6):774~786.
    杨宝俊,穆石敏,金旭,等.1996.中国满洲里—缓芬河地学断面地球物理综合研究.地球物理学报,39:772~782.
    杨宝俊,唐建人,李勤学,刘财,等.2001.松辽盆地深部反射地震探查.地球物理学进展,16(4):11~17.
    杨宝俊,李勤学,唐建人,等.2003.松辽盆地反射地震莫霍面的形态、三瞬处理结构及其地质解释.地球物理学报,46(3):398~402.
    杨卓欣,张先康,嘉世旭,等.2006.伽师强震群区震源细结构的深地震反射探测研究.地球物理学报,49(6):1701~1708.
    杨文采,程振炎,陈国九,等.1999a.苏鲁超高压变质带北部地球物理调查(I):深反射地震.地球物理学报,42(1):41~52.
    杨文采,胡振远,程振炎,倪诚昌,方慧,白金.1999b.郯城-涟水综合地球物理剖面.地球物理学报,42(2):206~217.
    姚保华,章振铨,王家林,等.2007.上海地区地壳精细结构的综合地球物理探测研究.地球物理学报,50(2):482~491.
    尹安.2001.喜马拉雅—青藏高原造山带地质演化—显生宙亚洲大陆生长.地球学报,22(3):193~230.
    袁学诚,徐明才,唐文榜,王庆海.1994.东秦岭陆壳反射地震剖面.地球物理学报,37:613~620.
    袁学诚,任纪舜,徐明才,唐文榜.2002.东秦岭邓县—南漳反射地震剖面及其构造意义.中国地质,29(1):14~19.
    曾融生,阚荣举.1961.柴达木盆地西部地壳深界面的反射波.地球物理学报,10(2):120~125.
    曾融生,陆涵行,丁志峰.1988.从地震折射和反射剖面讨论唐山地震成因.地球物理学报,31:383~398.
    张先康,宋建立.1994.深部地球物理研究及其在地震预报中的作用.地震学刊,4:36~40.
    张先康,王椿镛,刘国栋,等.1996.延庆—怀来地区地壳细结构——利用深地震反射剖面.地球物理学报,39:350~356.
    张先康,赵金仁,刘国华,等.2002.三河-平谷8.0级大震区震源细结构的深地震反射探测研究.中国地震,18(4):326~336.
    张贻侠,孙运生,张兴洲,等.1999.中国满洲里—绥芬河地学断面1:1000000说明书.北京:地质出版社.
    赵文津,Nelson K D,纳尔逊.1996a.印度板块俯冲到藏南之下的深反射证据.地球学报,17(2):131~137.
    赵文津,Nelson K D,车敬凯,等.1996b.深反射地震揭示喜马拉雅地区地壳上地幔的复杂结构.地球物理学报,39(5):615~628.
    赵文津,纳尔逊,车敬凯,等.1996c.喜马拉雅地区深反射地震——揭示印度大陆北缘岩石圈的复杂结构.地球学报,17(2):138~152.
    赵文津,徐中信,熊嘉育.1997.雅鲁藏布江缝合带的深部结构和构造.地质科技,29~33.
    赵文津,赵逊,史大年,刘葵,等.2002.喜马拉雅和青藏高原深剖面(I NDEPTH)研究进展.地质通报,21(11):691~700.
    赵文津,吴珍汉,史大年,等.2008.国际合作I NDEPTH项目横穿青藏高原的深部探测与综合研究.地球学报,29(3):328~342.
    赵金仁,张先康,张成科,等.2004.利用宽角反射/折射和深反射探测剖面揭示三河—平谷大震区深部结构特征.地球物理学报,47(4):646~653.
    朱金芳,徐锡伟,张先康,等.2005.福州盆地及邻区地壳精细结构的深地震反射与高分辨率折射及宽角反射/折射联合探测研究.中国科学(D辑),35(8):738~749.
    朱金芳,方盛明,张先康,等.2006.泉州盆地及其邻区地壳深部结构的探测与研究.中国地震,22(3):249~258.
    Abramoritz T,Thybo H,MONALISA Working Group.1998.Seismic structure across the Caledonian Deformation Frontalong MONALISA profile1in southeastern North Sea.Tectonophysics,288:153~176.
    All mendinger R W,Nelson K D,Potter C J,et al.1987.Deepseismic reflection characteristics of the continental crust.Geology,15:304~310.
    Ross A R,Brown L D,Pananont P,Nelson KD,Klemperer S.2004.Deep reflection surveying in central Tibet:lower-crustallayering and crustal flow.Geophys.J.Int.,156:115~128.
    Behr HJ,Heinrichs T.1987.Geological interpretation of DEKORP2-S:a deep seismic reflection profile across the Saxothuringianand possible i mplications for the Late Variscan structuralevolution of Central Europe.Tectonophysics,142(2~4):173~202.
    Behrmann J,Drozdzewski G,Heinrichs T,Huch M,et al.1991.Crustal-scale balanced cross sections through the Variscan foldbelt,Germany:the central EGT-segment.Tectonophysics,196(1~2):1~21.
    Balling N.2000.Deep seismic refection evidence for ancientsubduction and collision zones within the continental lithosphereof northwestern Europe.Tectonophysics,329:269~300
    Bois C,CAZES M,HIRN A,MASCLE A,MATTE P,et al.1988.Contribution of deep seismic profilingtothe knowledge ofthe lower crust in France and neighbouring areas.Tectonophysics,145:253~275.
    Bois C,ECORS Scientific Party.1990.Major geodynamic processesstudies from the ECORS deep seismic profiles in France andadjacent areas.Tectonophysics,173:397~410.
    Bois C.1991.Geological significance of seismic reflections incollision belts.Geophys.J.Int.,105:55~69.
    Bonjer K P.1997.Seismicity pattern and style of seismic faulting atthe eastern borderfault of the southern Rhine Graben.Tectonophysics,275(1~3):41~69.
    Brown L,Barazangi M,Kauf man S,Olicer J.1986.The firstdecade of COCORP:1974~1984.In:Barazangi M,Brown LD,eds.Reflection Seismology,A Global Perspective.GeodynSer.,13:107~120.
    Brown L D,Wille D M,et al.1987.COCORP:new perspectives onthe deep crust.Geophys.J.R.Astr Soc.,89:47~54.
    Brun J P,Gustcher M A,DEKORP-ECORS teama.1992.Deepcrustal structure of the Rhine Groben from DECORP-ECORSseismic reflection data:a summary.Tectonophysics,208:139~147.
    Chadwick R A,Pharaoh T C.1998.The seismic reflection Mohobeneath the United Kingdom and adjacent areas.Tectonophysics,299:255~279.
    Clowes R M.1992.LITHOPROBE:an integrated approach tostudies of crustal evolution.Geoti mes,Agu:12~14.
    Clowes R M,et al.1999.Canada's LITHOPROBE project(Collaborative,multidisciplinary geoscience research leads tonew understanding of continental evolution).Episodes,22(1):3~20.
    Clowes R M,Buriyank MJ A,Gorman A R,Kanasewich E R.2002.Crustal velocity structure from SAREX,the southernAlberta refraction experi ment.Canadian Journal of EarthSciences,39(3):351~373.
    Cook F A,van der Velden AJ,Hall K W.1999.Frozen subductionin Canada's Northwest Territories:lithoprobe deep lithosphericreflection profiling of the western Canadian Shield.Tectonics,18(1):1~24.
    Cook F A.2002.Fine structure of the continental reflection Moho.Geological Society of America Bulletin,114:64~79.
    Davey F J,Henyey T,et al.1998.Preli minary results from ageophysical study across a modern,continent-continentcollisional plate boundary-the Southern Alps,New Zealand.Tectonophysics,288:221~235.
    Davis J L,Bennett R A.2003.Assessment of GPS velocity accuracyfor the Basin and Range Geodetic Network(BARGEN).Geophysical Research Letters,30(7):1411.
    Eaton D W.2005.Multigenetic origin of the continental Moho:insights from LITHOPROBE.Terra Nova,18(1):34~43.
    Dehler S A,Clowes R M.1992.Integrated geophysical modeling ofterranes and other structural features along the westernCanadianmargin.Can.J.Earth Sci.,9:1492~1508.
    Dewey J,Kempton M,Kidd W,et al.1986.Shortening ofcontinental lithosphere:the neotectonics of eastern Analolia—ayoung collision zone.In:Coward M,Ries A,eds.CollisionTectonics.3~36.
    DEKORP Research Group.1990.Results of deep-seismic reflectioninvestigations inthe Rhenish Massif.Tectonophysics,173:507~515.
    DEKORP-BASI N Research Group,Krawczyk C M.1998.Surveyprovides insights into an old suture zone.EOS,79(12):151~159.
    DEKORP,Orogenic Processes Working Groups.1999a.Exhumationof subducted crust the Saxonian granulites from reflectionseismic experi ment GRANU'95.Tectonics,18:756~773.
    DEKORP,Orogenic Processes Research Groups,Krawczyk C M,correspondent.1999b.Structure of the Saxothuringiangranulites:geological and geophysical constraints on theexhumation of high-pressure/high-temperature rocks in themid-European Variscan belt.Tectonics,18(5):756~773.
    DEKORP-BASI N Research Group,Krawczyk C M,McCann T.1999c.The deep crustal structure of the Northeast Germanbasin:new DEKORP-BASI N'96deep-profiling results.Geology,27(1):55~58.
    Dong S W,Li QS,Gao R,et al.2008.Mcho-mappinginthe Dabieultrahigh pressure collisional orogen,central China.Am.J.Sci.,308(4):517~528.
    Drummond B J,Goleby B R.1993.Seismic reflection i mages ofmajor ore-controlling structures in the eastern Goldfields,Western Australia.Expl.Geophys.,24:473~478.
    Drummond B J,Goleby B R,Goncharov A G,et al.1997.Crustal-scale structures in the Proterozoic Mount Isa inlier of north Australia:their seismic response and influence onmineralisation.Tectonophysics,288:43~56.
    Drummond B J,Goleby B R,Owen A J,et al.2000.Seismicreflection i maging of mineral systems:three case histories.Geophysics,65:1852~1861.
    Drummond B,Lyons P,et al.2006.Constraining models of thetectonic setting of the giant Olympic Damiron oxide copper golddeposit,South Australia,using deep seismic reflection data.Tectonophysics,420:91~103.
    Goulty N.1993.Controlled-source tomography for mining andengineering application.In:Iyer H M,Hirahara K,eds.Seismic Tomography:Theory and Practice.London:Chapmanand Hall,797~813.
    Eisbacher G H,Lüschen E,Wickert F.1989.Crustal-scalethrusting and extension in the Hercynian Schwarzwald andVosges,Central Europe.Tectonics,8(1):1~21.
    Federal agency of mineral resources.2005.The Main Goals andAreas of Activity of Rosnedra.
    Finetti I R,Boccaletti M,Bonini M,del Ben A,Geletti R,PipanM,Sani F.2001.Crustal section based on CROP seismic dataacross the North Tyrrhenian Northern Apennines Adriatic Sea.Tectonophysics,343:135~163.
    Finetti I R.2004.Innovative CROP seismic highlights on theMediterranean region.Special Volume of the Italian GeologicalSociety for the IGC32Florence.131~140.
    Feng R,McErilly T V.1983.Interpretation of seismic reflectionprofiling data for the structure of the San Andreas fault zone.Bull.Seis.Soc.Am.,73:1701~1720.
    Fuis G S.1998.West margin of North America—a synthesis ofrecent seismic transects.Tectonophysics,288:262~292.
    Gao Rui,Huang Dongding,Lu Deyuan.1999.Deep seismicreflection profiles across contact zone of West Kunlun andTari mbasin along the Xinjiang geotransect in NWChina.TerraNostra,2(99):49~50.
    Gao Rui,Huang Dongding,Lu Deyuan,et al.2000.Deep seismicreflection profiles across juncture zone between Tari mbasin andwest Kunlun Mountain.Chinese Science Bulletin,45(17):1874~1849.
    Gao Rui,Li Pengwu,et al.2001.Deep process of the collision anddeformation on the northern margin of the Tibetan plateau:Revelation from investigation of the deep seismic profiles.Science in China(Series D),44:71~78.
    Gao Rui,Zen Lingsen,Zhu Xuan,Wang Haiyan,Feng Shaoying,Zhang Jisheng,Li Qiusheng,Li Pengwu,Lu zhanwu,LiuJinkai,Li Wenhui.2009.Lithosphere structures of thenortheastern margin of the Qinghai-Tibet plateau:geodynamici mplication for the deep processes that shaping the plateaumargin.5thInternational Symposiumon the Tibetan Plateau&24th Hi malaya-Karakorum-Tibet Workshop Abstracts,8,88~89.
    Giese P,Scheuber E,Schilling F,Schmitz M,Wigger P.1999.Crustal thickening processes in the Central Andes and the different natures of the Moho-discontinuity.J.of SouthAmerican Earth Sciences,12:201~220.
    Geoffrey Blewitt.2008.Fixed point theorems of GPS carrier phaseambiguity resolution and their application to massive networkprocessing.Ambizap Journal of Geophysical Research,113:B12410.
    Hale L D,Thompson S A.1982.The seismic reflection character ofthe continental Mohorovicic discontinuity.J.Geophys.Res.,87:4625~4635.
    Hammer P T C,Clowes R T.1997.Moho reflectivity patterns—acomparison of Canadian LITHOPROBE Transects.Tectonophysics,269:179~198.
    Hetzel R,Echtler H P,Seifert W,et al.1998.Subduction-andexhumation-related fabrics in the Paleozoic high-P/low-TMaksyutov Complex,Antingan area,southern Urals,Russia.Geological Society of America Bulletin,110:916~930.
    Holbrook WS,Brocher T M,Ten Brink US,et al.1996.Crustalstructure of a transformplate boundary:San Francisco Bay andthe central California continental margin.J.Geophys.Res.,101:22311~22334.
    Korsch RJ,Schafer A.1995.The Permo-Carboniferous Saar-Nahebasin,south-west Germany and north-east France:basinformation and deformation in a strike-slip regi me.GeologischeRundschau,84(2):293~318.
    Klemperer S L,Borwn L D,Oliver J E,et al.1985.Some results ofCOCORP seismic reflection profiling in the GreenvilleageAdiron-dack Mountains.J.Earth Sci.,22:141~153.
    Lemiszki PJ,Brown L D.1988.Variable crustal structure of strike-slip fault zones as observed on deep seismic reflection profiles.Geological Society of America Bulletin,100:665~676.
    Li Yuan Hsiao,Stephan A,Nat Tilander.2004.Seismic reflectioni maging of a major strike-slip fault zone in a rift system:Paleogene structure and evolution of the Tan-Lu fault system,Liaodong Bay,Bohai,offshore China.AAPG Bulletin,88(1):71~97.
    Oliver J.1993.COCORP probes continental depths.Geoti mes,June:21~22.
    Oncken O.1997.Transformation of a magmatic arc and an orogenicroot during oblique collision and its conseq-uences for theevolution of the European Variscides(Mid-German CrystallineRise).Geol.Rdsch,86:2~20.
    Oncken O.1998a.Orogenic mass transfer and reflection seismicpatterns-evidence from DEKORP sections across the EuropeanVariscides(central Germany).Tectonophysics,286:47~61.
    Oncken O.1998b.Evidence for precollisional subduction erosion inancient collisional belts:The case of the Mid-EuropeanVariscides.Geology,26(12):1075~1078.
    Patro P K,Egbert G D.2008.Regional conductivity structure ofCascadia:preli minary results from3D inversion of USArraytransportable array magnetotelluric data.Geophysical ResearchLetters,35:L20311.
    Matthews D H,The BIRPS Group.1990.Progress in BIRPS deep seismic reflection profiling around the British Isles.Testonophysics,173:387~396.
    Meier L,Eisbacher G H.1991.Crustal kinematics and deepstructure of the northern Rhine Graben,Germany.Tectonics,10(3):621~630.
    Meissner R.1989.Rupture creep,lamellae and crocodiles happeningsin the continental crust.Tera nova,1:17~28.
    Meissner R,Wever Th.1986.Nature and development of the crustaccording to deep reflection data fromthe German Variscides.In:Reflection Seismology:A Global Perspective,eds.M.Barazangi and L.D.Brown.Geodyn.Ser,13:31~42.
    Meissner R,Wever Th,Sadowiak P.1991.Continental collisionsand seismic signature.Geophy.J.Int.,105:15~23.
    Meissner R,Wever Th.1996.Nature and development of the crustaccording to deep reflection data fromthe German Variscides.In:Barazangi M,Brown L D,eds.Reflection Seismology:AGlobal Perspective.Washington DC,Am Geophys.Union,Geodyn.Ser.,13:31~42.
    Moss F J,Mathur S P.1986.A review of continental reflectionprofiling in Australia.In:Barazangi M,Brown L D,eds.Reflection seismology;A Global Perspective.AmericanGeophysical Union Geodynamics Series,13:67~76.
    Morgan J V,Hadwin M,Warner MR,et al.1994.The polarity ofdeep seismic reflections fromthe lithosphere mantle:evidencefor a relict seduction zone.Tectonophysics,232:319~328.
    Nelson K D.1991.A unfied view of craton evolution motivated byrecent deep seismic reflection and refraction results.Geophy.J.Int.,105:25~35.
    Norris R J,Koons P O,Cooper A L.1990.The obliquelyconvergent plate boundary in the South Island of New Zealandini mplications for ancient collision zones.J.Struct.Geol.,12:715~725.
    Rousset D,Bayer R,Guillon D,Edel J B.1993.Structure of thesouthern Rhine Graben fromgravity and reflection seismic data(ECORS-DEKORP program).Tectonophysics,221(2):135~153.
    Schmid R,Ryberg T,Ratschbacher L,et al.2001.Crustalstructure of the eastern Dabie Shan interpreted from deepreflection and shallow tomographic data.Tectonophysics,333(3~4):347~359.
    Steer D N,Knapp J H,Brown L D,Echtler H P,Prz-Estaun A,Berzin R.1998.Deep structure of the continental lithosphereinan unextended orogen:an explosive source seismic reflectionprofile in the Urals(Urals Seismic Experi ment and IntegratedStudies(URSEIS1995).Tectonics,17:143~157.
    Sadowiak P,Wever T,Meissner R.1991.Deep seismic reflectivitypatterns in specific tectonic units of western and central Europe.Geophy.J.Int.,105:45~54.
    Spencer C,Thurlow G,Wright J,et al.1993.Avibroseis reflectionsurvey at the Buchans mine in central Newfo-undland.Geophysics,58:154~166.
    Verpaelst P,Peloquin AS,Adam E,et al.1995.Seismic reflection profiling across the“Mine Series”in the Noranda camp of theAbitibibelt,eastern Canada.Can.J.Earth Sciences,32:167~176.
    Vernicke B.1985.Uniform sense si mple shear of the continentallithosphere.Can.J.Earth Sci.,22:108~125.
    Wallace R E.1990.The San Andreas fault system.California.United States Government Printing Office,Washington.
    Warner M,Morgan J,Barton P,et al.1996.Seismic reflectionsfromthe mantle represent relict subduction zones within thecontinental lithosphere.Geology,24:39~42.
    Weng S,Chen H,Zhou X,Cui Z.1990.Deep seismic probing ofcontinental crust in the Lower Yangtze region,eastern China,Tectonophysics,173:297~305.
    Xiong Xiaosong,Gao Rui,Li Qiusheng,Lu Zhanwu.2009.TheMoho depth of Qinghai-Tibet plateau revealed by seismic probe.Journal of Earth Science,4:448~463.
    Yang Y J,Ritzwoller M H.2008.Teleseismic surface wavetomographyinthe western U.S.usingthe Transportable Arraycomponent of USArray.Geophysical Research Letters,35,L04308.
    Yoon M,Buske S,Shapiro S A,Wigger P.2009.Reflectioni magespectroscopy across the Andean subduction zone.Tectonophysics,472:51~61.
    Zhao WJ,Nelson K D,Project Team.1993.Deep seismic reflectionevidence for continental underthrusting beneath southern Tibet.Nature,366:557~559.

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