引文
[1]陈社发,邓起东,赵小麟,等.龙门山中段推覆构造带及相关构造的演化历史和变形机制(一)[J].地震地质,1994,16(4):404-412.Chen S F,Deng Q D,Zhao X L,et al.Deformationalcharacteristics,Evolutionary history,and Deformationmechanism of the middle Longmenshan Thrust-Nappes andrelated tectonics[J].Seismology and Geology(in Chinese),1994,16(4):404-412.
[2]许志琴,李化启,侯立玮,等.青藏高原东缘龙门-锦屏造山带的崛起-大型拆离断层和挤出机制[J].地质通报,2007,26(10):1262-1276.Xu Z Q,Li H Q,Hou L W,et al.Uplift of the Longmen-Jinping orogenic belt along the eastern margin of the Qinghai-Tibet Plateau:Large-scale detachment faulting and extrusionmechanism[J].Geological Bulletin of China(in Chinese),2007,26(10):1262-1276.
[3]邓起东,陈社发,赵小麟.龙门山及其邻区的构造和地震活动及动力学[J].地震地质,1994,16(4):389-403.Deng Q D,Chen S F,Zhao X L.Tectonics,Scismisity anddynamics of Longmenshan mountains and its adjacent regions[J].Seismology and Geology(in Chinese),1994,16(4):389-403.
[4]陈国光,许凤桔,周荣军,等.龙门山断裂带晚第四纪活动性分段的初步研究[J].地震地质,2007,29(3):657-673.Chen G G,Xu F J,Zhou R J,et al.Primary research ofactivity segmentation of Longmenshan Fault Zone since Late-Quaternary[J].Seismology and Geology(in Chinese),2007,29(3):657-673.
[5]Wu M L,Zhang Y Q,Liao C T,et al.Preliminary results ofin-situ stress measurements along the Longmenshan fault zoneafter the Wenchuan MS8.0Earthquake[J].Acta GeologicaSinica,2009,83(4):746-753.
[6]Dirks P H G M,Wilson C J L,Chen S,et al.Tectonicevolution of the NE margin of the Tibetan Plateau:evidencefrom the central Longmen Mountains,Sichuan Province,China[J].J.Southeast Asian Earth Sci.,1994,9(1-2):181-192.
[7]Chen S F,Wilson C J L,Worley B A.Tectonic transitionfrom the Songpan-Garzêfold belt to the Sichuan Basin,South-western China[J].Basin Res.,1995,7(3):235-253.
[8]Chen S,Wilson C J L.Emplacement of the Longmenmountain thrust-nappe belt along the eastern margin of theTibetan Plateau[J].Journal of Structural Geology,1996,18(4):413-430.
[9]刘树根,罗志立,戴苏兰,等.龙门山冲断带的隆升和川西前陆盆地的沉降[J].地质学报,1995,69(3):205-214.Liu S G,Luo Z L,Dai S L,et al.The uplift of theLongmenshan thrust belt and subsidence of the westernSichuan foreland Basin[J].Acta Geologica Sinica(inChinese),1995,69(3):205-214.
[10]金文正,汤良杰,杨克明,等.川西龙门山褶皱冲断带分带性变形特征[J].地质学报,2007,81(8):1073-1080.Yu W Z,Tang L J,Yang K M,et al.Deformation andzonation of the Longmenshan fold and thrust zone in theWestern Sichuan Basin[J].Acta Geologica Sinica(inChinese),2007,81(8):1073-1080.
[11]李智武,刘树根,陈洪德,等.龙门山冲断带分段-分带性构造格局及其差异变形特征[J].成都理工大学学报(自然科学版),2008,35(4):440-454.Li Z W,Liu S G,Chen H D,et al.Structural segmentationand zonation and differential deformation across and along theLongmen thrust belt,West Sichuan,China[J].Journal ofChengdu University of Technology(Science&TechnologyEdition)(in Chinese),2008,35(4):440-454.
[12]楼海,王椿镛,姚志祥,等.龙门山断裂带深部构造和物性分布的分段特征[J].地学前缘,2010,17(5):128-141.Lou H,Wang C Y,Yao Z X,et al.Subsection feature of thedeep structure and material properties of Longmenshan Faultzone[J].Earth Science Frontiers(in Chinese),2010,17(5):128-141.
[13]郭正吾,邓康龄,韩永辉.四川盆地形成与演化[M].北京:地质出版社,1996.Guo Z W,Deng K L,Han Y H.Formation and Evolution ofSichuan Basin[M].Beijing:Geological Publishing House(inChinese),1996.
[14]Jia D,Wei G Q,Chen Z X,et al.Longmen Shan fold-thrustbelt and its relation to the western Sichuan Basin in centralChina:New insights from hydrocarbon exploration[J].AAPG Bulletin,2006,90(9):1425-1447.
[15]Arne D,Worley B,Wilson C,et al.Differential exhumationin response to episodic thrusting along the eastern margin ofthe Tibetan Plateau[J].Tectonophysics,1997,280(3-4):239-256.
[16]邓康龄.龙门山构造带印支期构造递进变形与变形时序[J].石油与天然气地质.2007,28(4):485-490.Deng K L.Indosinian progressive deformation and itschronogenesis in Longmengshan structural belt[J].Oil&Gas Geology(in Chinese),2007,28(4):485-490.
[17]罗志立,龙学明.龙门山造山带崛起和川西陆前盆地沉降[J].四川地质学报,1992,12(1):1-17.Luo Z L,Long X M.The uplifting of The Longmenshanorogenic zone and the subsidence of the west Sichuan forelandbasin[J].Acta Geologica Sichuan(in Chinese),1992,12(1):1-17.
[18]王治顺,朱大岗,熊成云,等.构造体系各论(中国典型构造体系分论)[M].北京:地质出版社,1999.Wang Z S,Zhu D G,Xiong C Y,et al.Separate Treatises onTectonic Systems(Individual papers on typical tectonicsystems of China)[M].Beijing:Geological PublishingHouse(in Chinese),1999.
[19]罗志立,金以钟,朱夔玉,等.试论上扬子地台的峨眉地裂运动[J].地质评论,1988,34(1):11-24.Luo Z L,Jin Y Z,Zhu K Y,et al.On Emei Taphrogenesisof the upper Yangtze Platform[J].Geological Review(inChinese),1988,34(1):11-24.
[20]周荣军,蒲晓虹,何玉林,等.四川岷江断裂带北段的新活动、岷山断块的隆起及其与地震活动的关系[J].地震地质,2000,22(3):285-294.Zhou R J,Pu X H,He Y L,et al.Recent activity ofMinjiang fault zone,uplift of Minshan block and theirrelationship with seismicity of Sichuan[J].Seismology andGeology(in Chinese),2000,22(3):285-294.
[21]赵小麟,邓起东,陈社发.岷山隆起的构造地貌学研究[J].地震地质,16(4):429-439.Zhao X L,Deng Q D,Chen S F.Tectonic Geomorphology ofthe Minshan uplift in Western Sichuan,Southwestern China[J].Seismology and Geology(in Chinese),16(4):429-439.
[22]唐荣昌,文德华,黄祖智,等.松潘-龙门山地区主要活动断裂带第四纪活动特征[J].中国地震,1991,7(3):64-71.Tang R C,Wen D H,Huang Z Z,et al.The Quaternaryactivity characteristics of several major active faults in theSongpan-Longmenshan Region[J].Earthquake Research inChina(in Chinese),1991,7(3):64-71.
[23]文德华.龙门山北段断裂活动特征[J].四川地震,1994,(1):53-57.Wen D H.Activity characteristic of North Longmenshanfault zone[J].Earthquake Research in Sichuan(in Chinese),1994,(1):53-57.
[24]李传友,宋方敏,冉勇康.龙门山断裂带北段晚第四纪活动性讨论[J].地震地质,2004,26(2):248-25.Li C Y,Song F M,Ran Y K.Late quaternary activity andage constraint of the northern Longmenshan fault zone[J].Seismology and Geology(in Chinese),2004,26(2):248-25.
[25]李勇,黄润秋,周荣军,等.龙门山地震带的地质背景与汶川地震的地表破裂[J].工程地质学报,2009,17(1):3-18.Li Y,Huang R Q,Zhou R J,et al.Geological background ofLongmen Shan seismic belt and surface ruptures in Wenchuanearthquake[J].Journal of Engineering Geology(in Chinese),2009,17(1):3-18.
[26]李勇,周荣军,Densmore A L,等.青藏高原东缘大陆动力学过程与地质响应[M].北京:地质出版社,2006:1-134.Li Y,Zhou R J,Densmore A L,et al.Continental dynamicprocesses and geological response in the Eastern Margin ofthe Qinghai-Tibet Plateau[M].Beijing:GeologicalPublishing House(in Chinese),2006:1-134.
[27]Densmore A L,Ellis M A,Li Y,et al.Active tectonics ofthe Beichuan and Pengguan faults at the eastern margin of theTibetan Plateau[J].Tectonics,2007,26(4):TC4005.
[28]徐锡伟,闻学泽,叶建青,等.汶川MS8.0地震地表破裂带及其发震构造[J].地震地质,2008,30(3):597-629.Xu X W,Wen X Z,Ye J Q,et al.The MS8.0 Wenchuanearthquake surface ruptures and its seismogenic structure[J].Seismology and Geology(in Chinese),2008,30(3):597-629.
[29]陈运泰,许力生,张勇,等.2008年5月12日汶川特大地震震源特性分析报告——初步考察成果(一).2008.http://www.eq-igp.ac.cn/汶川地震专题/初步研究与考察结果(一).Chen Y T,Xu L S,Zhang Y,et al.Source characteranalysis report of Wenchuan Earthquake on may 12,2008--Preliminary investigated results(in Chinese).http://www.eq-igp.ac.cn
[30]Klee G,Rummel F,Williams A.Hydraulic fracturing stressmeasurements in Hong Kong[J].International Journal ofRock Mechanics and Mining Sciences,1999,36(6):731-741.
[31]Hickman S H,Zoback M D,Healy J H.Continuation of adeep borehole stress measurement profile near the SanAndreas Fault-1.Hydraulic fracturing stress measurementsat Hi Vista,Mojave Desert,California[J].Journal ofGeophysical Research,1988,93(B12):15183-15195.
[32]Townend J,Zoback M D.Regional tectonic stress near theSan Andreas Fault in central and southern California[J].Geophys.Res.Lett.,2004,31,L15S11,doi:10.1029/2003GL018918.
[33]Tembe S,Lockner D,Wong T F.Constraints on the stressstate of the San Andreas Fault with analysis based on coreand cuttings from San Andreas Fault Observatory at Depth(SAFOD)drilling phases 1and 2[J].J.Geophys.Res.,2009,114,B11401,doi:10.1029/2008JB005883.
[34]陈群策,丰成君,孟文,等.5.12汶川地震后龙门山断裂带东北段现今地应力测量结果分析[J].地球物理学报,2012,55(12):3923-3932.Chen Q C,Feng C J,Meng W,et al.Analysis of in situstress measurements at the northeastern section of theLongmenshan fault zone after the 5.12 Wenchuanearthquake[J].Chinese J.Geophys.(in Chinese),2012,55(12):3923-3932.
[35]孟文,陈群策,杜建军,等.新加坡地应力测量[J].地球物理学报,2012,55(8):2611-2619.Meng W,Chen Q C,Du J J,et al.In-situ stressmeasurement in Singapore[J].Chinese J.Geophys.(inChinese),2012,55(8):2611-2619.
[36]杨树新,姚瑞,崔效锋,等.中国大陆与各活动地块、南北地震带实测应力特征分析[J].地球物理学报,2012,55(12):4207-4217.Yang S X,Yao R,Cui X F,et al.Analysis of thecharacteristics of measured stress in Chinese mainland and itsactive blocks and North-South seismic belt[J].Chinese J.Geophys.(in Chinese),2012,55(12):4207-4217.
[37]李四光.论地震[M].北京:地质出版社,1977.Li S G.The Earthquake[M].Beijing:Geological PublishingHouse(in Chinese),1977.
[38]Zoback M D,Healy J H.In-situ stress measurements to 3.5km depth in Cajon.Pass Scientific Research Bore-hole:implications for the mechanics of crustal faulting[J].J.G.R.,1992,97(B4):5039-5057.
[39]Zoback M D,Healy J H.Friction,faulting and“in situ”stress[J].Annales Geophysicae,1984,2(6):689-698.
[40]Byerlee J O.Friction of rocks[J].Pure and Applied Geophysics,1978,116(4-5):615-626.
[41]戴黎明,李三忠,陶春辉,等.印度板块挤压驱动龙门山断裂带活动的三维数值模型[J].地球物理学进展,2011,26(1):41-51.Dai L M,Li S Z,Tao C H,et al.Three-dimensionalnumberical modeling of activity of the Longmenshan faultzone driven by the India Plate[J].Progress in Geophysics(inChinese),2011,26(1):41-51.
[42]刘健,熊探宇,赵越,等.龙门山活动断裂带运动学特征及其构造意义[J].吉林大学学报(地球科学版),2012,42(sup.2):320-330.Liu J,Xiong T X,Zhao Y,et al.Kinematic characteristicsof Longmenshan active fault zone and its tectonic implication[J].Journal of Jilin University(Earth Science Edition)(inChinese),2012,42(sup.2):320-330.
[43]崔效锋,胡幸平,俞春泉,等.汶川地震序列震源机制解研究[J].北京大学学报(自然科学版),2011,47(6):1063-1072.Cui X F,Hu X P,Yu C Q,et al.Research on focalmechanism solutions of wenchuan earthquake sequence[J].Acta Scientiarum Naturalium Universitatis Pekinensis(inChinese),2011,47(6):1063-1072.
[44]Royden L H,Burchfiel B C,King W R,et al.Surfacedeformation and lower crustal flow in eastern Tibet[J].Science,1997,276(5313):788-790.
[45]Clark M K,Royden L H.Topographic ooze:Building theeastern margin of Tibet by lower crustal flow[J].Geology,2000,28(8):703-706.
[46]Meng Q R,Wang E,Hu J M.Mesozoic sedimentary evolution ofthe northwest Sichuan Basin:implication for continuedclockwise rotation of the South China Block[J].GeologicSociety of American Bulletin,2005,117(3):396-410.
[47]Burchfiel B C,Chen Z L,Liu Y P,et al.Tectonics of theLongmen Shan and adjacent regions,central China[J].International Geology Review,1995,37(8):661-735.
[48]Harris N.Channel flow and the Himalayan-Tibetan orogen:a critical review[J].Journal of the Geological Society,2007,164(3):511-523.
[49]Lou H,Wang C Y.Wavelet analysis and interpretation ofgravity data in Sichuan-Yunnan region,China[J].ActaSeismologica Sinica,2005,18(5):552-561.