引文
①张凤旭.松辽盆地南部综合地球物理剖面研究(内部研究报告).2009.
[1]张贻侠,孙运生,张兴洲,等.中国满洲里—绥芬河地学断面1∶1000000说明书[M].北京:地质出版社,1998.Zhang Yi-xia,Sun Yun-sheng,Zhang Xing-zhou,etal.Manual on the Geosciences Transect fromManzhouli to Suifenghe,China(1∶1 000 000)[M].Beijing:Geological Publishing House,1998.
[2]水谷伸治郎,邵济安,张庆龙.那丹哈达地体与东亚大陆边缘中生代构造的关系[J].地质学报,1989,63(3):204-215.Mizutani S,Shao Ji-an,Zhang Qing-long.The Rela-tionship of the Nadanhada Terrane and MesozoicStructure of Continental Margin in East Asia[J].ActaGeologica Sinica,1989,63(3):204-215.
[3]曹熹,党增欣,张兴洲,等.佳木斯复合地体[M].长春:吉林科学出版社,1992.Cao Xi,Dang Zeng-xin,Zhang Xing-zhou,et al.Jia-musi Composite Terrane[M].Changchun:JilinSciences and Technology Press,1992.
[4]杨宝俊.在地学断面域内用地震学方法研究大陆地壳:以中国满洲里—绥芬河地学断面为例[M].北京:地质出版社,1999.Yang Bao-jun.Studying of Continental Crust UsingSeismological Method in the Zone of Geoscience Tran-sect:Manzhouli-Suifenhe Geoscience Transect of China[M].Beijing:Geological Publishing House,1999.
[5]杨宝俊,穆石敏,金旭,等.中国满洲里—绥芬河地学断面地球物理综合研究[J].地球物理学报,1996,39(6):772-782.Yang Bao-jun,Mu Shi-min,Jin Xu,et al.SynthesizedStudy on the Geophysics of Manshouli-Suifenhe Geo-science Transect,China[J].Chinese J Goephys,1996,39(6):772-782.
[6]杨宝俊,唐建仁,李勤学,等.松辽盆地深部反射地震探查[J].地球物理学进展,2001,16(4):11-17.Yang Bao-jun,Tang Jian-ren,Li Qin-xue,et al.DeepSeismic Reflection Probing in Songliao Basin[J].Pro-gress in Geophysics,2001,16(4):11-17.
[7]杨宝俊,刘万崧,王喜臣,等.中国东部大兴安岭重力梯级带域地球物理特征及其成因[J].地球物理学报,2005,48(1):86-97.Yang Bao-jun,Liu Wan-song,Wang Xi-chen,et al.Geophysical Characteristics of Daxing’anling Gravita-tional Gradient Zone in the East China and Its Geody-namic Mechanism[J].Chinese J Geophys,2005,48(1):86-97.
[8]刘国兴,张兴洲,杨宝俊,等.佳木斯地块及东边缘岩石圈电性结构特征[J].地球物理学报,2006,49(2):598-603.Liu Guo-xing,Zhang Xing-zhou,Yang Bao-jun,et al.Electrical Structures of the Lithosphere Along the Jia-musi Massif and Its Eastern Edge[J].Chinese J Geo-phys,2006,49(2):598-603.
[9]刘财,张兴洲,刘洋,等.东北跃进山拼贴带及邻域岩石圈结构特征的地电学证据[J].地球物理学报,2009,52(4):958-965.Liu Cai,Zhang Xing-zhou,Liu Yang,et al.Geoelec-trical Evidence for Characteristics of LithosphericStructure Beneath the Yuejinshan Collage Zone and ItsVicinity in Northeast Asia[J].Chinese J Geophys,2009,52(4):958-965.
[10]刘财,杨宝俊,王兆国,等.松辽盆地西边界带深部构造:地电学证据[J].地球物理学报,2011,54(2):401-406.Liu Cai,Yang Bao-jun,Wang Zhao-guo,et al.TheDeep Structure of the Western Boundary Belt of theSongliao Basin:The Geoelectric Evidence[J].Chi-nese J Geophysics,2011,54(2):401-406.
[11]刘财,杨宝俊,王兆国,等.大兴安岭西北部中新生代盆地群基底电性分带特征研究[J].地球物理学报,2011,54(2):415-421.Liu Cai,Yang Bao-jun,Wang Zhao-guo,et al.AResearch on the Geoelectrical Banding Characteristicsof the Bottom of the Mesozoic-Cenozoic Basin Groupsin the Northwest of the Da Hinggan Ling Fault[J].Chinese J Geophysics,2011,54(2):415-421.
[12]杨宝俊,张梅生,王璞珺.中国油气田地质-地球物理解析:上卷[M].北京:科学出版社,2003.Yang Bao-jun,Zhang Mei-sheng,Wang Pu-jun.Geo-logical-Geophysics Analytic Interpretation on Oil andGas Potential Region of China:Volume I[M].Bei-jing:Science Press,2003.
[13]Sun J.On the Limited Aperture Migration in TwoDimensions[J].Geophysics,1998,63:984-994.
[14]Sun J.3-D Crosswell Transmissions:Paraxial RaySolutions and Reciprocity Paradox[J].Geophysics,1995,60:810-820.
[15]Sun J.Limited Aperture Migration[J].Geophysics,2000,65:584-595.
[16]Sun J.Ture-Amplitede Weight Function in 3DLimi-ted-Aperture Migration Revisited[J].Geophysics,2004,69(4):1025-1036.
[17]Liu Y,Liu C,Wang D.A 1DTime-Varying MedianFilter for Seismic Random,Spike-Like Noise Elimina-tion[J].Geophysics,2009,74:17-24.
[18]Liu C,Liu Y,Yang B J,et al.A 2D Multistage Me-dian Filter to Reduce Random Seismic Noise[J].Geo-physics,2006,71(5):105-110.
[19]刘财,李红星,陶春辉,等.模糊嵌套多级中值滤波方法及其在地震数据处理中的应用[J].地球物理学报,2007,50(5):1534-1542.Liu Cai,Li Hong-xing,Tao Chun-hui,et al.A NewFuzzy Nesting Multilevel Filter and Its Application toSeismic Data Processing[J].Chinese J Geophys,2007,50(5):1534-1542.
[20]李月,林洪波,杨宝俊,等.强随机噪声条件下时窗类型局部线性化对TFPF技术的影响[J].地球物理学报,2009,52(7):1899-1906.Li Yue,Lin Hong-bo,Yang Bao-jun,et al.The Influ-ence of Limited Linearization of Time Window on TF-PT Under the Strong Noise Back Ground[J].ChineseJ Geophys,2009,52(7):1899-1906.
[21]Deng X Y,Yang D H,Peng J M,et al.Noise Re-duction and Drift Removal Using Least-Squares Sup-port Vector Regression with the Implicit Bias Term[J].Geophysics,2010,75(6):119-127.
[22]邓小英,杨顶辉,刘涛,等.最小二乘支持向量回归滤波系统性能分析[J].地球物理学报,2010,53(8):2004-2044.Deng Xiao-ying,Yang Ding-hui,Liu Tao,et al.Per-formance Analysis of Least Squares Support VectorRegression Filtering System[J].Chinese J Geophys,2010,53(8):2004-2044.
[23]邓小英,刘涛,罗勇.Ricker子波核最小二乘支持向量回归滤波方法的鲁棒性研究[J].地球物理学报,2011:54(3):845-853.Deng Xiao-ying,Liu Tao,Luo Yong.Robustness ofLeast Squares Support Vector Regression FilteringMethod with Ricker Wavelet Kernel[J].Chinese JGeophys,2011:54(3):845-853.
[24]Liu Y,Fomel S.OC-Seislet Transform Constructionwith Differential Continuation[J].Geophysics,2010,75(6):235-245.
[25]刘洋,Fomel S,刘财,等.高阶seislet变换及其在随机噪声消除中的应用[J].地球物理学报,2009,52(8):2142-2151.Liu Yang,Fomel,Liu Cai,et al.Hign-Order SeisletTransform and Its Application of Random Noise At-tenuation[J].Chinese J Geophys,2009,52(8):2142-2151.
[26]Wu N,Li Y,Yang B J,et al.Application of theTrace Transform in Surface Wave Attenuation onSeismic Records[J].IEEE Transactions on Geosci-ences and Remote Sensing,2011,49(12):4997-5007.
[27]Wu N,Li Y,Yang B J,et al.Surface WaveAttenuation of Seismic Records with the Co-CoreTrace Transform Filter[J].Geophysics,2011,76(6):115-128.
[28]刘财,郭志奇,杨宝俊,等.黏弹各向异性介质中波的反射与透射问题分析[J].地球物理学报,2007,50(4):1216-1224.Liu Cai,Guo Zhi-qi,Yang Bao-jun,et al.Analysisof Reflection an Transmission of Waves in Viscoelas-tic Anisotropic Media[J].Chinese J Geophys,2007,50(4):1216-1224.
[29]李月,杨宝俊.检测强噪声背景下周期信号的混沌系统[J].科学通报,2003,48(1):19-20.Li Yue,Yang Bao-jun.Chaotic System for the Detec-tion of Periodic Signal Under the Background ofStrong Noise[J]Chinese Science Bulletin,2003,48(1):19-20.
[30]李月,杨宝俊,袁野.混沌振子检测系统的弱有效地震信号检测能力[J].科学通报,2006,51(14):1710-1716.Li Yue,Yang Bao-jun,Yuan Ye,et al.Ability to De-tect Weak Effect-Tive Seismic Signals by UtilizingChaotic Vibrator[J].Chinese Science Bulletin,2006,51(14):3010-3017.
[31]Li Y,Yang B J,Bada J,et al.Chaotic System Detec-tion of Weak Seismic Signals[J].Geophys J Int,2009,178:1493-1522.
[32]李月,杨宝俊,林洪波,等.地震勘探时空双曲滤波因子的特点与提高信噪比的能力[J].地球物理学报,2008,51(5):1557-1566.Li Yue,Yang Bao-jun,Lin Hong-bo,et al.Charac-teristics of Hyperbolic Time Distance Relation Filterin Seismic Prospecting and Its Ability Increasing Sig-nal-to-Noise Ratio[J].Chinese J Goephys,2008,51(5):1557-1566.
[33]Feng X,Motoyuki S,Zhang Y,et al.CMP AntennaArray GPR and Signal-to-Clutter Ratio Improvement[J].IEEE Geoscienc and Remote Sensing Letters,2009,6(1):23-27.
[34]Feng X,Motoyuki S,Liu C,et al.Profiling theRough Surface by Migration[J].IEEE Geosciencand Remote Sensing Letters,2009,6(2):258-262.
[35]Feng X,Motoyuki S,Liu C,et al.Hand-Held GPRImaging Using Migration for Irregular Data[J].IEEEJournal of Selected Topics in Applied Earth Observa-tions and Remote Sensing,2011,4(4):799-803.
[36]单玄龙,秦树洪,张艳,等.松辽盆地北部浅部基底推覆伸展作用的地震学证据与地质意义[J].地球物理学报,2009,52(8):2044-2049.Shan Xuan-long,Qin Shu-hong,Zhang Yan,et al.Seismic Evidence an Geological Significance ofThrust-Extension Structure in Upper Basemeng onNorth Songliao Basin[J].Chinese J Geophys,2009,52(8):2044-2049.
[37]郑亚东,王士政,王玉芳.中蒙边境区新发现的特大型推覆构造及伸展变质核杂岩[J].中国科学:B辑,1990,20(12):1299-1305.Zheng Ya-dong,Wang Shi-zheng,Wang Yu-fang.The New Discovery of Mega Thrusting Tectonics andMetamorphic Core Complexes in the Boundary of Chi-na and Mongolia[J].Science in China:Series B,1990,20(12):1299-1305.
[38]郑亚东,Davis G A,王琮,等.内蒙古大青山大型逆冲推覆构造[J].中国科学:D辑,1998,28(4):289-295.Zheng Ya-dong,Davis G A,Wang Cong,et al.Study on Daqingshan Mega Thrusting Tectonics inInner Mongolia[J].Science in China:Series D,1998,28(4):289-295.
[39]和政军,李锦轶,牛宝贵,等.燕山—阴山地区晚侏罗世强烈推覆:隆升事件及沉积响应[J].地质论评,1998,44(4):407-418.He Zheng-jun,Li Jin-yi,Niu Bao-gui,et al.A LateJutassic Intense Thrusting-Uplifting Event in theYanshan-Yinshan Area,Northern China,and ItsSedimentary Response[J].Geological Review,1998,44(4):407-418.
[40]Yang B J,Liu C,Han L G,et al.A Study of De-tachment Faults of the Upper Crust in Manzhouli-Suifenhe GGT by the Method of Vertical Seismic Re-flection[C]//Liu G D.Proceedings of the 30th Inter-national Geological Congress.Utrecht:VSP,1997:51-61.
[41]刘财,孟令顺,吴燕冈,等.东北地球物理场与地壳演化[M].北京:地质出版社,2009.Liu Cai,Meng Ling-shun,Wu Yan-gang,et al.Geo-physical Field and Frustal Evolution in the FortheastChina[M].Beijing:Geological Publishing House,2009.
[42]Zhao W J,Nelson K D,Che J,et al.Deep FeismicFeflection Evidence for Continental UnderthrustingBeneath Southern Tibet[J].Nature,1993,366:557-559.
[43]Nelson K D,Zhao W J,Brown L D,et al.PartiallyMolten Middle Crust Beneath Southern Tibet:Syn-thesis of Project INDEPTH Results[J].Science,1996,274:1684-1688.
[44]Bostock M G.Seismic Imaging of Lithospheric Dis-continuities and Continental Evolution[J].Lithos,1999,48:1-16.
[45]Jordan T H.Composition and Development of theContinental Tectosphere[J].Nature,1978,274:544-548.
[46]魏斯禹,滕吉文,王谦身,等.中国东部大陆边缘地带的岩石圈结构与动力学[M].北京:科学出版社,1990:177-187.Wei Si-yu,Teng Ji-wen,Wang Qian-shen,et al.Dy-namics and Lithospheric Tectonic of Continental Mar-gin Zone in East China[M].Beijing:Science Press,1990:177-187.
[47]Khan M A.Comparative Evaluation of Recent GlobalRepresentations of Earth’s Gravity Field[J].GeophyJ R Astro Soc,1976,46:535-553.
[48]杨宝俊,刘万崧.大兴安岭—太行山—武陵山重力梯级带的成因[J].长春科技大学学报,2000,30(增刊):23-25.Yang Bao-jun,Liu Wan-song.The Formation of theGravitative Gradient Zone Along Daxinganling Moun-tain-Taihangshan Mountain-Wulingshan Mountain[J].Journal of Changchun University of Science andTechnology,2000,30(Sup.):23-25.
[49]Anderson D L.Top-Down Tectonics?[J].Science,2001,293:2016-2018.
[50]Anderson D L.The Thermal State of the UpperMantle:No Role for Mantle Plumes[J].GeophysRes Lett,2000,27:3623.
[51]King S D,Ritsema J.African Hotspot Volcanism:Small-Scale Convection in the Upper Mantle BeneathCratons[J].Science,2000,290:1137-1140.
[52]McNutt M K,Caress D W,Reynolds J,et al.Failureof Plume Theory to Explain Midplate Volcanism inthe Southern Austral islands[J].Nature,1997,389:479-482.
[53]Stein M,Hofmann A W.Mantle Plumes and EpisodicCrustal Growth[J].Nature,1994,372:63-68.
[54]杨宝俊,李勤学,唐建人,等.松辽盆地反射地震莫霍面的形态、三瞬处理结果及其地质解释[J].地球物理学报,2003,46(3):398-402.Yang Bao-jun,Li Qin-xue,Tang Jian-ren,et al.TheForm and Three-Instantaneous Information of theSeismic Reflection Moho in Songliao Basin and Geo-logical Interpretation[J].Chinese J Geophys,2003,46(3):398-402.
[55]杨宝俊,唐建人,李勤学,等.松辽盆地隆起区地壳反射结构与“断开”莫霍界面[J].中国科学:D辑,2003,33(2):170-176.Yang Bao-jun,Tang Jian-ren,Li Qin-xue,et al.Crustal Reflection Structure in the Uplifting Zone ofSongliao Basin and Disconnecting Moho Interface[J].Science in China:Series D,2003,33(2):170-176.
[56]曾融生.莫霍面界面的性质[J].地球物理学报,1964,13(2):180-188.Zeng Rong-sheng.Nature of Moho Interface[J].Chinese J Geophys,1964,13(2):180-188.
[57]朱夏.试论中国中新生代油气盆地的地球动力学背景[C]//朱夏.论中国含油气盆地构造.北京:石油工业出版社,1986:61-70.Zhu Xia.Review on Geodynamic Background of Oiland Gas Basin of Mesozoic and Neozoic Era in China[C]//Zhu Xia.Chinese Tectonics of Oil and Gas-Bearing Basin.Beijing:Petroleum Industry Press,1986:61-70.