引文
[1]郝天珧,刘伊克,段昶.中国东部及其领域地球物理场特征与大地构造意义.地球物理学报,1997,40(5):677-690Hao T Y,Liu Y K,Duan C.The characteristic of geophysical fieldin the East China and adjacent regions and its tectonics significance.Chinese J.Geophys.(in Chinese),1997,40(5):677-690
[2]邓起东.鄂尔多斯周缘断陷盆地的构造活动特征及其形成机制.见:国家地震局地质研究所.现代地壳运动研究1.——大陆裂谷与深部过程.北京:地震出版社,1985.58-78Deng Q D.Tectonic movement characteristics and its formingmechanism of the faulted basins along the margins of Ordos.In:Institute of Geology,China Earthquake Administration.The Studieson Modern Crust MovementⅠ.——Continental Rifts and PlutonicProcesses(in Chinese).Beijing:Seismological Press,1985.58-78
[3]许忠淮,汪素云,高阿甲.地震活动反映的青藏高原东北地区现代构造运动特征.地震学报,2000,22(5):472-481Xu Z H,Wang S Y,Gao A J.Present-day tectonic movement inthe northeastern margin of the Qinghai-Xizang(Tibetan)Plateau asrevealed by earthquake activity.Acta Seismologica Sinica(inChinese),2000,22(5):472-481
[4]邓起东,程绍平,闵伟等.鄂尔多斯块体新生代构造活动和动力学的讨论.地质力学学报,1999,5(3):13-21Deng Q D,Cheng S P,Min W,et al.Discussion on Cenozoictectonics and dynamics of Ordos block.Journal of Geomechanics(inChinese),1999,5(3):13-21
[5]徐锡伟,程国良,马杏垣等.华北及其邻区地体转动模式和动力来源.地球科学-中国地质大学学报,1994,19(2):130-138Xu X W,Cheng G L,Ma X Y,et al.Rotation model and dynamicsof blocks in North China and its adjacent areas.Earth Science-Journal of China University of Geoscience(in Chinese),1994,19(2):130-138
[6]Zhang Y Q,Mercier J L,Vergely P.Extension in the graben systemaround the Odors(China),and its contribution to the extrusiontectonics of south China with respect to Gobi-Mongolia.Tectonophysics,1998,285:41-75
[7]Peltzer G,Saucier F.Present-day kinematics of Asia derived fromgeologic fault rates.J Geophys R,1996,101(B12):27943-27956
[8]叶加仁,赵鹏大,陆明德等.鄂尔多斯盆地下古生界油气地质动力学研究.中国科学(D辑),2000,30(1):40-46Ye J R,Zhao P D,Lu M D,et al.Petroleum geological dynamics ofLower Paleozoic in the Ordos Basin northwest China.Science inChina(Series D)(in Chinese),2000,30(1):40-46
[9]Zhang Y Q,Vergely P,Mercier J L.Active faulting in and along theQinling Range(China)inferred from SPOT imagery analysis andextrusion tectonics of southern China.Tectonophysics,1995,243:69-95
[10]李曙光,孙卫东,张国伟等.南秦岭勉略构造带黑沟峡变质火山岩的年代学和地球化学.中国科学(D辑),1996,26(3):223-230Li S G,Sun W D,Zhang G W,et al.Chronology and geochemistryof metavolcanic rocks from Heigouxia Valley in the Mian-Luetectonic zone,South Qinling-evidence for a Paleozoic oceanic basinand its close time.Science in China(Series D)(in Chinese),1996,26(3):223-230
[11]张国伟,郭安林,姚安平.中国大陆构造中的西秦岭—松潘大陆构造结.地学前缘,2004,11(3):23-32Zhang G W,Guo A L,Yao A P.Western Qinling-Songpancontinental tectonic node in China’s continental tectonics.EarthScience Frontiers(in Chinese),2004,11(3):23-32
[12]丁燕云.鄂尔多斯盆地北部航磁异常反映的构造特征.物探与化探,2000,24(3):197-202Ding Y Y.Structural characteristics of northern Ordos basin reflectedby aeromagnetic data.Geophyscial and Geochemical Exploration(inChinese),2004,11(3):23-32
[13]张家声,李燕,韩竹均.青藏高原向东挤出的变形响应及南北地震带构造组成.地学前缘,2003,10(增刊):168-175Zhang J S,Li Y,Han Z J.Deformation responses to eastwardsescaping of the Qinghai-Tibet plateau and tectonics of the south-northseismic zones in China.Earth Science Frontiers(in Chinese),2003,10(Suppl.):168-175
[14]赵国春,孙敏,Wilde S A.华北克拉通基底构造单元特征及早元古代拼合.中国科学(D辑),2002,32(7):538-549Zhang G C,Sun M,Wilde S A.Major tectonic units of the NorthChina Craton and their Paleoproterozoic assembly.Science in China(Series D)(in Chinese),2002,32(7):538-549
[15]伍家善,耿元生,沈其韩等.中朝古陆地质特征及构造演化.北京:地质出版社,1998.1-212Wu J S,Geng Y S,Shen Q H,et al.Geological characteristics andtectonic evolutions of the Sino-Korean Block(in Chinese).Beijing:Geological Publishing House,1998.1-212
[16]贾进斗,何国琦,李茂松等.鄂尔多斯盆地基底结构特征及其古生界天然气的控制.高校地质学报,1997,3(2):144-153Jia J D,He G Q,Li M S,et al.Structural feature of basement inthe Ordos basin and its control to Paleozoic gas.Geological Journal ofChina Universities(in Chinese),1997,3(2):144-153
[17]张渝昌等.中国含油气盆地原型分析.南京:南京大学出版社,1997.262-294Zhang Y C,et al.Prototype analysis of petroliferous basins in China(in Chinese).Nanjing:Nanjing University Press,1997.262-294
[18]吴昌华,李树勋,高吉风等.华北克拉通太古代和早元古代变质区.见:董申保主编.中国变质作用及其与地壳演化的关系.北京:地质出版社,1986.53-89Wu C H,Li S X,Gao J F,et al.Archaean-early proterozoicmetamorphic terrains in the North China craton.In:Dong S B ed.China Metamorphism and the Relations Between It and the Earth’sCrust’s Evolvement(in Chinese).Beijing:Geological PublishingHouse,1986.53-89
[19]嘉世旭,张先康.华北不同构造块体地壳结构及其对比研究.地球物理学报,2005,48(3):611-620Jia S X,Zhang X K.Crustal structure and comparison of differenttectonic blocks in North China.Chinese J.Geophys.(in Chinese),2005,48(3):611-620
[20]贾承造,施央申,郭令智.东秦岭板块构造.南京:南京大学出版社,1988Jia C Z,Shi Y S,Guo L Z.Plate Tectonics of the East Qinling(inChinese).Nanjing:Nanjing University Press,1988
[21]张国伟,张宗清,董云鹏.秦岭造山带主要构造岩石地层单元的构造性质及其大地构造意义.岩石学报,1995,11(2):101-114Zhang G W,Zhang Z Q,Dong Y P.Nature of main tectono-lithostratigraphic units of the Qinling Orogen:implications for thetectonic evolution.Acta Petrologica Sinica(in Chinese),1995,11(2):101-114
[22]张国伟,孟庆任,刘少峰等.华北地块南部巨型陆内俯冲带与秦岭造山带岩石圈现今三维结构.高校地质学报,1997,3(2):129-143Zhang G W,Meng Q R,Liu S F,et al.Huge intracontinentalsubduction zone at south margin of North China block and present 3-D lithospheric framework of the Qinling orogenic belt.GeologicalJournal of China Universities(in Chinese),1997,3(2):129-143
[23]孙晓猛,吴根耀,郝福江等.秦岭-大别造山带北部中新生代逆冲推覆构造期次及时空迁移规律.地质科学,2004,39(1):63-76Sun X M,Wu G Y,Hao F J,et al.Epochs and space-timemigrating of meso-cenozoic thrust-nappe tectonics in the northQinling-Dabie orogen.Chinese Journal of Geology(in Chinese),2004,39(1):63-76
[24]张国伟,董云鹏,赖绍聪等.秦岭-大别造山带南缘勉略构造带与勉略缝合带.中国科学(D辑),2003,33(12):1121-1135Zhang G W,Dong Y P,Lai S C,et al.Mian-Lue tectonic zoneand Mian-Lue ductile shear zone in the south margin of Qinling-Dabie orogen.Science in China(Series D)(in Chinese),2003,33(12):1121-1135
[25]Burchfiel B C.New Technology;New Geological Challenges.GSAToday,2004,14(2):4-10
[26]Chris Wijns,Carlos Perez,Peter Kowalczyk.Theta map:Edgedetection in magnetic data.Geophysics,2005,70:39-43
[27]Roest W,Verhoef J,Pilkington M.Magnetic interpretation using the3-D analytic signal.Geophysics,1992,57:116-125
[28]谢新生.旋卷构造应力场与鄂尔多斯地块周缘断裂系成因探讨.地震学报,2004,26(4):419-425Xie X S.Discussion on rotational tectonic stress field and the genesisof Circum-Ordos landmass fault system.Acta Seismologica Sinica(inChinese),2004,26(4):419-425
[29]Tapponnier P,Molnar P.Active faulting and tectonics in China.Journal of Geophysical Research,1977,82:2905-2930
[30]Xu X,Ma X.Geodynamics of the Shanxi rift system,China.Tectonophysics,1992,208:325-340
[31]Northrup C J,Rpyden L H,Burchfiel B C.Motion of the Pacificplate relative to Eurasia and its potential relation to Cenozoicextension along the eastern margin of Eurasia.Geology,1995,23(8):719-722
[32]Tian Z Y,Han P,Xu K D.The Mesozic-Cenozoic East China riftsystem.Tectonophysics,1992,208:341-363
[33]张国伟,郭安林,刘福田等.秦岭造山带三维结构及其动力学分析.中国科学(D辑),1996,26(增刊):1-6Zhang G W,Guo A L,Liu F T,et al.Three-dimensionalarchitecture and dynamic analysis of the Qinling Orogenic Belt.Science in China(Series D)(in Chinese),1996,26(Suppl.):1-6
[34]Xue F,Lerch M F,Kroner A,et al.Tectonic evolution of the eastQinling mountains,China,in the palaeozoic;A review and a newtectonic model.Tectonophysics,1996,235:271-284
[35]张世民.汾渭地堑系盆地发育进程的差异及其控震作用.地质力学学报,2000,6(2):30-37Zhang S M.Basin evolutionary differences and seismotectonics ofFenwei graben system.Journal of Geomechanics(in Chinese),2000,6(2):30-37
[36]何建坤,刘福田,刘建华等.东秦岭造山带莫霍面展布与碰撞造山带深部过程的关系.地球物理学报,1998,41(增刊):64-76He J K,Liu F T,Liu J H,et al.The morphology of Mohodiscontinuity and it’s evolution geodynamics in the Eastern Qinlingcollisional orogenic belt.Chinese J.Geophys.(in Chinese),1998,41(Suppl.):64-76
[37]徐果明,李光品,王善恩等.用瑞利面波资料反演中国大陆东部地壳上地幔横波速度的三维构造.地球物理学报,2000,43(3):366-376Xu G M,Li G P,Wang S E,et al.The 3-D structure of shear wavesin the crust and mantle of east continental China inverted by Rayleighwave data.Chinese J.Geophys.(in Chinese),2000,43(3):366-376