引文
[1]马保起,苏刚,侯治华,等.利用岷江阶地的变形估算龙门山断裂带中段晚第四纪滑动速率[J].地震地质,2005,27(2):234-242.Ma B Q,Su G,Hou Z H,et al.Late quaternary slip rate inthe central part of the Longmenshan fault zone from terracedeformation along the Minjiang river[J].Seismology andGeology(in Chinese),2005,27(2):234-242.
[2]陈国光,计凤桔,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,Ji 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.
[3]王阎昭,王恩宁,沈正康,等.基于GPS资料约束反演川滇地区主要断裂现今活动速率[J].中国科学D辑:地球科学,2008,38(5):582-597.Wang Y Z,Wang E N,Shen Z K,et al.Inversed presentactive rate of main faults of Sichuan and Yunnan base on GPSdata[J].Science China(Series D):Earth Sciences(inChinese),2008,38(5):582-597.
[4]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 characters of faults in the north ofLongmenshan[J].Earthquake Research in Sichuan(inChinese),1994,(1):53-57.
[5]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.
[6]余团,何昌荣.龙门山构造带区域稳定性探讨[J].地震研究,2000,23(4):378-383.Yu T,He C R.Research on the regional stability along thestructural belt in Longmen mountains[J].Journal ofSeismological Research(in Chinese),2000,23(4):378-383.
[7]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):248-258.Li C Y,Song F M,Ran Y K.Late quaternary activity and ageconstraint of the northern Longmenshan fault zone[J].Seismology and Geology(in Chinese),2004,26(2):248-258.
[8]AKI K.Asperities,barriers,characteristic earthquakes andstrong motion prediction[J].J.Geophys.Res.,1984,89(B7):5867-5872.
[9]张国民,邵志刚,刘桂萍,等.汶川8.0级地震构造动力成因分析[J].地震,2009,29(1):164-173.Zhang G M,Shao Z G,Liu G P,et al.Analysis on thegeodynamic cause of the Wenchuan 8.0 earthquake[J].Earthquake(in Chinese),2009,29(1):164-173.
[10]王小亚,朱文耀,符养,等.GPS监测的中国及其周边现时地壳形变[J].地球物理学报,2002,45(2):198-209.Wang X Y,Zhu W Y,Fu Y,et al.Present-time crustaldeformation in china and its surrounding regions by GPS[J].Chinese J.Geophys.(in Chinese),2002,45(2):198-209.
[11]武艳强,江在森,杨国华,等.汶川地震前GPS资料反映的应变率场演化特征[J].大地测量与地球动力学,2011,31(5):20-25.Wu Y Q,Jiang Z S,Yang G H,et al.Evolutioncharacteristics of strain rate field reflected by GPS data beforeWenchuan earthquake[J].Journal of Geodesy andGeodynamics(in Chinese),2011,31(5):20-25.
[12]张希,崔笃信,王文萍,等.利用GPS资料分析汶川地震前后川滇及其邻区水平运动及应变积累[J].地震研究,2008,31(增刊):464-470.Zhang X,Cui D X,Wang W P,et al.Using gps data toanalyze horizontal movement and strain accumulation inSichuan-Yunnan and its vicinity before and after theWenchuan earthquake[J].Journal of Seismological Research(in Chinese),2008,31(Supp.):464-470.
[13]张希,蒋锋云,崔笃信,等.四川及邻区GPS观测揭示的应变积累与大震影响分析[J].大地测量与地球动力学,2011,31(5):9-13.Zhang X,Jiang F Y,Cui D X,et al.Analysis of strainaccumulation and influence of great earthquake observed byGPS in Sichuan and its adjacent areas[J].Journal of Geodesyand Geodynamics(in Chinese),2011,31(5):9-13.
[14]杨晓平,冯希杰,戈天勇,等.龙门山断裂带北段第四纪活动的地质地貌证据[J].地震地质,2008,30(3):644-657.Yang X P,Feng X J,Ge T Y,et al.Geological andgeomorphic evidence for the quaternary activity on thenortheast segment of Longmenshan fault zone[J].Seismology and Geology(in Chinese),2008,30(3):644-657.
[15]陈立春,陈杰,刘进峰,等.龙门山前山断裂北段晚第四纪活动性研究[J].地震地质,2008,30(3):710-722.Chen L C,Chen J,Liu J F,et al.Investigation of latequaternary activity along the northern range-front fault,Longmenshan[J].Seismology Geology(in Chinese),2008,30(3):710-722.
[16]李方全.1976年唐山大震的地应力测量[J].地壳构造与地壳应力,2010,(1):34-36.Li F Q.Stress measurement of Tangshan 1976earthquake[J].Crustal Tectonic and Crustal Stress(in Chinese),2010,(1):34-36.
[17]Liao C T,Zhang C S,Wu M L,et al.Stress change near theKunlun fault before and after the MS8.1Kunlun earthquake[J].Geophysical Research Letters,2003,30(20):20-27.
[18]徐锡伟,张培震,闻学泽,等.川西及其邻近地区活动构造基本特征与强震复发模型[J].地震地质,2005,27(3):446-461.Xu X W,Zhang P Z,Wen X Z,et al.Features of activetectonics and recurrence behaviors of strong earthquakes inthe western Sichuan province and its adjacent regions[J].Seismology and Geology(in Chinese),2005,27(3):446-461.
[19]张培震.青藏高原东缘川西地区的现今构造变形、应变分配与深部动力过程[J].中国科学D辑,2008,38(9):1041-1056.Zhang P Z.The tectonic deformation,strain distribution anddeep dynamic process in the eastern margin of the Qinghai-Tietan plateau[J].Science in China(Series D)(in Chinese),2008,38(9):1041-1056.
[20]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(增刊2):320-330.Liu J,Xiong T Y,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.
[21]杨长清,刘树根,曹波,等.龙门山造山带与川西前陆盆地耦合关系及其对油气成藏的控制[J].成都理工大学学报(自然科学版),2008,35(4):471-476.Yang C Q,Liu S G,Cao B,et al.Basin-range couplingsystem and its control on oil and gas accumulation in theLongmen orogenic belt and the West Sichuan foreland basin[J].Journal of Chengdu of University of Technology(Science&Technology Edition)(in Chinese),2008,35(4):471-476.
[22]田小彬.龙门山北段构造特征及油气前景探讨[硕士论文].四川:成都理工大学,2009.Tian X B.Structural features in the northern segment ofLongmen Mountains and the discussion on its hydrocarbonprospects(in Chinese)[Master’s thesis].Sichuan:ChengduUniversity of Technology,2009.
[23]罗志立.龙门山造山带的崛起和四川盆地的形成与演化[M].成都:成都科技大学出版社,1994:288-303.Luo Z L.The uplifting of the Longmenshan orogenic zoneand evolution history of the Sichuan basin(in Chinese)[M].Chengdu:Chengdu University of Science and TechnologyPress,1994:288-303.
[24]许志琴,杨经绥,姜枚,等.大陆俯冲作用及青藏高原周缘造山带的崛起[J].地学前缘,1999,6(3):139-151.Xu Z Q,Yang J S,Jiang M,et al.Continental subductionand uplifting of the orogenic belts at the margin of theQinghai-Tibet plateau[J].Earth Science Frontiers(inChinese),1999,6(3):139-151.
[25]Molnar P.Mio-pliocene growth of the Tibetan plateau andevolution of east Asian climate[J].PalaeontologiaElectronica,2005,8(1):1-23.
[26]尹安.喜马拉雅-青藏高原造山带地质演化――显生宙亚洲大陆生长[J].地球学报,2001,22(3):193-230.Yin A.Geologic evolution of the Himalayan-Tibetan orogenin the context of phanerozoic continental growth of Asia[J].Acta Geoscientica Sinica(in Chinese),2001,22(3):193-230.
[27]Molnar P,Englang P,Martionod J.Mantle dynamics,upliftof the Tibetan plateau,and the Indian monsoon[J].Reviewsof Geophysics,1993,31(4):357-396.
[28]齐少华,刘启元,陈九辉,等.汶川MS8.0地震:龙门山断裂两侧地壳各向异性的初步研究[J].地震地质,2009,31(3):377-388.Qi S H,Liu Q Y,Chen J H,et al.Wenchuan earthquakeMS8.0:preliminary study of crustal anisotroph on bothsides of the Longmenshan faults[J].Seismology and Geology(in Chinese),2009,31(3):377-388.
[29]任治坤,田勤俭,陈立泽.南北地震带中段地震构造遥感解译[J].地震,2005,25(4):127-132.Ren Z K,Tian Q J,Chen L Z.Seismotectonic interpretationalong central section of Chinese north-south seismic belt fromETM image[J].Earthquake(in Chinese),2005,25(4):127-132.
[30]樊春,王二七,王刚,等.龙门山断裂带北段晚新近纪以来的右行走滑运动及其构造变换研究-以青川断裂为例[J].地质科学,2008,43(3):417-433.Fan C,Wang E Q,Wang G,et al.Dextral strike-slip andtectonic transformation of the northern Longmen Shan faultbelt from late neogene:a case study from the Qingchuan fault[J].Chinese Journal of Geology(in Chinese),2008,43(3):417-433.
[31]江娃利,张景发,谢新生,等.建立在雷达卫星影像判读基础上四川龙门山断裂带晚第四纪活动特征研究[J].第四纪研究,2009,29(3):426-438.Jiang W L,Zhang J F,Xie X S,et al.Late quaternaryactivity characteristics of Longmenshan fault zone in Sichuanbased on SAR satellite image interpretation[J].QuaternarySciences(in Chinese),2009,29(3):426-438.
[32]路静,张景发,姜文亮,等.龙门山断裂带北段活动特征的遥感地质解译研究[J].地震,2009,29(增刊):164-172.Lu J,Zhang J F,Jiang W L,et al.Interpretation of activetectonics along the northern segment of the Longmenshanfault zone from RS images[J].Earthquake(in Chinese),2009,29(supp):164-172.
[33]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 MS8.10Wenchuanearthquake surface ruptures and its seismogenic structure[J].Seismology and Geology(in Chinese),2008,30(3):597-629.
[34]Zoback M D,Healy J H.In-situ stress measurements to 3.5km depth in the Cajon pass scientific research borehole:implications for the mechanics of crustal faulting[J].Journalof Geophysical Research,1992,97(B4):5039-5057.
[35]Haimson B C,Cornet F H.ISRM Suggested Methods forrock stress estimation-Part 3:hydraulic fracturing(HF)and/or hydraulic testing of pre-existing fractures(HTPF)[J].International Journal of Rock Mechanics and MiningSciences,2003,40(7-8):1011-1020.
[36]李方全,孙世宗,李立球.华北及郯庐断裂带地应力测量[J].岩石力学与工程学报,1982,1(1):73-86.Li F Q,Sun S Z,Li L Q.In-situ stress measurements inNorth China and Tancheng-Lujiang fault zone[J].ChineseJournal of Rock Mechanics and Engineering(in Chinese),1982,1(1):73-86.
[37]廖椿庭,吴满路,张春山,等.青藏高原昆仑山和羊八井现今地应力测量及其工程意义[J].地球学报,2002,23(4):353-358.Liao C T,Wu M L,Zhang C S,et al.Recent ground stressmeasurement of the Kunlun Mountains and Yangbajing areain Qinghai-Tibet Plateau and its engineering significance[J].Acta geoscientica Sinica(in Chinese),2002,23(4):353-358.
[38]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.
[39]郭啟良,王成虎,马洪生,等.汶川MS8.0级大震前后的水压致裂原地应力测量[J].地球物理学报,2009,52(5):1-7.Guo Q L,Wang C H,Ma H S,et al.In-situ hydro-fracturestress measurement before and after the Wenchuan MS8earthquake of China[J].Chinese J.Geophys.(in Chinese),2009,52(5):1-7.
[40]郭啟良,张彦山,王成虎,等.汶川地震构造断裂带的震前地壳深部原地应力测量[M].//汶川8.0级地震地壳动力学研究专辑.北京:地震出版社,2009.Guo Q L,Zhang Y S,Wang C H,et al.In-situ stressmeasurement in deep boreholes on the seismic faults beforeWenchuan earthquake[M].//Crustal dynamics of theWenchuan MS8.0 earthquake(in Chinese).Beijing:Seismological Press,2009.
[41]徐锡伟,陈桂华,于贵华,等.5.12汶川地震地表破裂基本参数的再论证及其构造内涵分析[J].地球物理学报,2010,53(10):2321-2336.Xu X W,Chen G H,Yu G H,et al.Reevaluation of surfacerupture parameters of the 5.12Wenchuan earthquake and itstectonic implication for Tibetan uplift[J].Chinese J.Geophys.(in Chinese),2010,53(10):2321-2336.
[42]李方全.断层活动与原地应力状态[M].//中国活动断层研究.北京:地震出版社,1994.Li F Q.Fault activity and in situ stress state[M].//Studyon China active faults(in Chinese).Beijing:Seismic Press,1994:15-21.
[43]Wu M L,Zhang Y Q,Liao C T,et al.Preliminary results ofin-situ stress measurements along the Longmenshan faultzone after the Wenchuan MS8.0 earthquake[J].ActaGeologica Sinica,2009,83(4):746-753.
[44]吴满路,张岳桥,廖椿庭,等.汶川地震后沿龙门山裂断带原地应力测量初步结果[J].地质学报,2010,84(9):1292-1299.Wu M L,Zhang Y Q,Liao C T,et al.Preliminary results ofin-situ stress measurements along the Longmenshan faultzone after the Wenchuan MS8.0 earthquake[J].ActaGeologica Sinica(in Chinese),2010,84(9):1292-1299.
[45]郭祥云,陈学忠,李艳娥.2008年5月12日四川汶川8.0级地震与部分余震的震源机制解[J].地震,2010,30(1):50-60.Guo X Y,Chen X Z,Li Y E.Focal mechanism solutions forthe 2008 MS8.0 Wenchuan earthquake and part of itsaftershocks[J].Earthquake(in Chinese),2010,30(1):50-60.
[46]安其美,丁立丰,王海忠,等.龙门山断裂带的性质与活动性研究[J].大地测量与地球动力学,2004,24(2):115-119.An Q M,Ding L F,Wang H Z,et al.Research of propertyand activity of Longmen mountain fault zone[J].Journal ofGeodesy and Geodynamics(in Chinese),2004,24(2):115-119.
[47]陈群策,安其美,孙东生,等.山西盆地现今地应力状态与地震危险性分析[J].地球学报,2010,31(4):541-548.Chen Q C,An QM,Sun D S,et al.Current in-situ stressstate of Shanxi basin and analysis of earthquake risk[J].ActaGeoscientica Sinica(in Chinese),2010,31(4):541-548.
[48]王凯英,Yu R,刁桂芩,等.2008年汶川地震前震源区的异常应力状态[J].地震地质,2012,34(1):11-16.Wang K Y,Yu R,Diao G L,et al.Stress state of Wenchuanarea before the 2008strong earthquake[J].Seismology andGeology(in Chinese),2012,34(1):11-16.