引文
[1]Zoback M D,Hickman S,Ellsworth W.The Role of Fault Zone Drilling[J].Geophysics,2007,4:649-674.
[2]Xu Z Q,Ji S C,Li H B,et al.Uplift of the Longmen Shan range and the Wenchuan earthquake[J].Episodes,2008,31(3):291-301.
[3]Brodsky E,Ma K F,Mori J,et al.Rapid response fault drilling:past,present and future.Report of the ICDP/SCEC International Workshop of Rapid Response Fault Drilling.Tokyo,Japan,2009,Nov.17-19.
[4]Oshiman N,Shimamoto T,Takemura K.et al.Thematic issue:Nojima fault zone probe[J].Island Arc,2001,10:195-505.
[5]Ma K F,Tanaka H,Song S R,et al.Slip zone and energetics of a large earthquake from the Taiwan Chelungpu-fault Drilling Project[J].Nature,2006,444(7118):473-476.
[6]Song S R,Kuo L W,Yeh E C,et al.Characteristics of the lithology,fault-related rocks and fault zone structures in the TCDP Hole-A[J].Terrestrial Atmospheric and Oceanic Science,2007,18:243-269.
[7]李海兵,付小方,Van D W,等.汶川地震(Ms8.0)地表破裂及其同震右旋斜向逆冲作用[J].地质学报,2008,82(12):1623-1643.Li Haibing,Fu Xiaofang,Van der Word,et al.Co-seisimic surface rupture and dextral-slip oblique thrusting of the Ms8.0Wenchuan earthquake[J].Acta Geological Sinica,2008,82(12):1623-1643(in Chinese with English abstract).
[8]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 Xiwei,Wen Xueze,Ye Jiangqing,et al.The Ms8.0Wenchuan earthquake surface ruptures and its seismogenic structure[J].Seismology and Geology,2008,30(3):597-629(in Chinese with English abstract).
[9]付碧宏,王萍,孔屏,等.四川汶川5_12大地震同震滑动断层泥的发现及构造意义[J].岩石学报,2008,24(10):2237-2243.Fu Bihong,Wang Ping,Kong Ping,et al.Preliminary study of coseismic fault gouge occurred in the slip zone of Wenchuan Ms8.0earthquake and its tectonic implicstions[J].Acta Petrologica Sinica,2008,24(10):2237-2243(in Chinese with English abstract).
[10]刘静,张智慧,文力,等.汶川8级大地震同震破裂的特殊性及构造意义[J].地质学报,2008,82(12):1707-1722.Liu Jing,Zhang Zhihui,Wen Li,et al.The Ms8.0Wenchuan earthquake co-seismic rupture and its tectonic implications:an out of sequence thrusting event with slip partitioned on multiple faults[J].Acta Geologica Sinica,2008,82(12):1707-1722(in Chinese with English abstract).
[11]李勇,周荣军,Densmore A L,等.映秀—北川断裂的地表破裂与变形特征[J].地质学报,2008,82(12):1688-1706.Li Yong,Zhou Rongjun,Densmore A L,et al.Surface rupture and deformation of the Yingxiu—Beichuan fault by the Wenchuan earthquake[J].Acta Geologica Sinica,2008,82(12):1688-1706(in Chinese with English abstract).
[12]李勇,周荣军,Densmore A L,等.青藏高原东缘龙门山晚新生代走滑-逆冲作用的地貌标志[J].第四纪研究,2006,26(1):40-52.Li Yong,Zhou Rongjun,Densmore A L,et al.Geomorphic evidence for the late Cenozoic strike-slipping and thrusting in Longmen Mountain at the eastern margin of the Tibetan Plateau[J].Quaternary Sciences,2006,26(1):40-51(in Chinese with English abstract).
[13]Burchfiel B C,Chen Z L,Liu Y,et al.Tectonics of the Longmen Shan and adjacent regions,Central China[J].International Geology Review,1995,37(8):661-735.
[14]Densmore A L,Ellis M A,Li Y,et al.Active tectonics of the Beichuan and Pengguan faults at the eastern margin of the Tibetan Plateau[J].Tectonics,2007,26(TC4005):doi:10.1029/2006TC001987.
[15]唐荣昌,韩渭宾.四川活动断裂与地震[M].北京:地质出版社,1993:1-190.Tang Rongchang,Han Weibin.Active Faults and Earthquake in Sichuan Province[M].Beijing:Geological Publishing House,1993:1-190(in Chinese).
[16]冯先岳.新疆古地震[M].乌鲁木齐:新疆科技卫生出版社,1997:228-229.Feng Xianyue.The Paleoearthquakes in Xinjiang Region,China[M].Urumqi:Xinjiang Science and Sanitary Press,1997:228-229(in Chinese).
[17]李海兵,司家亮,付小方,等.2008年汶川地震同震滑移特征、最大滑移量及构造意义[J].第四纪研究,2009,29(3):387-402.Li Haibing,Si Jialiang,Fu Xiaofang,et al.Co-seismic rupture and maximum displacement of the2008Wenchuan earthquake and its tectonic implications[J].Quaternary Sciences,2009,29(3):987-402(in Chinese with English abstract).
[18]Fu B H,Shi P L,Guo H D,et al.Surface deformation related to the2008Wenchuan earthquake,and mountain building of the Longmen Shan,eastern Tibetan Plateau[J].Journal of Asian Earth Sciences,2011,40(4):805-824.
[19]Xu X W,Wen X Z,Yu G H,et al.Coseismic reverse-and oblique-slip surface faulting generated by the2008Mw7.9Wenchuan earthquake,China[J].Geology,2009,37(6):515-518.
[20]Liu-Zeng J,Wen L,Sun J,et al.Surficial Slip and Rupture Geometry on the Beichuan Fault near Hongkou during the Mw7.9Wenchuan Earthquake,China[J].Bulletin of the Seismological Society of America,2010,100(5B):2615-2650.
[21]付碧宏,时丕龙,王萍,等.2008年汶川地震断层北川段的几何学与运动学特征及地震地质灾害效应[J].地球物理学报,2009,52(2):485-495.Fu Bihong,Shi Piping,Wang Ping,et al.Geometry and kinematics of the Wenchuan earthquake surface ruptures around the Qushan Town of Beichuan County,Sichuan:Implications for mitigation of seismic and geologic disasters[J].Chinese Journal of Geophysics,2009,52(2):485-495(in Chinese with English abstract).
[22]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[R].2008.http://www.csi.ac.cn.Chen Yuntai,Xu Lisheng,Zhang Yong,et al.Report on the great Wenchuan earthquake source of May12,2008[R].http://www.csi.ac.cn.
[23]张勇,冯万鹏,许力生,等.2008年汶川大地震的时空破裂过程[J].中国科学(D辑),2008,38(10):1186-1194.Zhang Yong,Feng Wanpeng,Xu Lisheng,et al.Spatio temporal rupture process of the2008great Wenchuan earthquake[J].Science in China(series D),2009,52,(2):145-154(in Chinese with English abstract).
[24]王卫民,赵连锋,李娟,等.四川汶川8.0级地震震源过程[J].地球物理学报,2008,51(5):1403-1410.Wang Weimin,Zhao Lianfeng,Li Juan,et al.2008.Rupture process of the Ms8.0Wenchuan earthquake of Sichuan,China[J].Chinese Journal of Geophysics,51(5):1403-1410(in Chinese with English abstract).
[25]Li C Y,Wei Z Y,Ye J Q,et al.Amounts and styles of coseismic deformation along the northern segment of surface rupture,of the2008Wenchuan Mw7.9earthquake,China[J].Tectonophysics,2010,491:35-58.
[26]四川省地矿局.灌县幅地质图(1:200000)[M].1975.Sichuan Bureau of Geology.Geologic map of Guangxian(scale1:200000)[M].1975(in Chinese).
[27]马永旺,王国芝,胡新伟.“彭灌杂岩”推覆体的构造变形特征[J].四川地质学报,1996,16(2):110-114.Ma Yongwang,Wang Guozhi,Hu Xinwei.Tectonic deformation of Pengguan complex as a nappe[J].Acta Geologica Sichuan,1996,16(2):110-114(in Chinese with English abstract).
[28]李勇,侯中健,司光影,等.青藏高原东缘新生代构造层序与构造事件[J].中国地质,2002,29(1):30-36.Li Yong,Hou Zhongjian,Si Guangying,et al.Cenozoic tectonic sequence and tectonic events at the eastern margin of the Qinghai-Tibet plateau[J].Geology in China,2002,29(1):30-36(in Chinese with English abstract).
[29]许志琴,李化启,侯立玮,等.青藏高原东缘龙门山-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 Zhiqin,Li Huaqi,Hou Liwei,et al.Uplift of the Longmen-Jinping orogenic belt along the eastern margin of the Qinghai-Tibet Plateau:Large-scale detachment faulting and extrusion mechanism[J].Geological Bulletin of China,2007,26(10):1262-1276(in Chinese with English abstract).
[30]Yan Q R,Hanson A D,Wang Z Q,et al.Neoproterozoic Subduction and Rifting on the Northern Margin of the yangtze Plate,China:Implications for Rodinia Reconstruction[J].International Geology Review,2004,46(9):817-832.
[31]Zhou M F,Yan D P,Wang C L,et al.Subduction-related origin of the750Ma Xuelongbao adakitic complex(Sichuan Province,China):Implications for the tectonic setting of the giant Neoproterozoic magmatic event in South China[J].Earth and Planetary Science Letters,2006,248(1-2):286-300.
[32]Sibson R H.Fault rocks and fault mechanisms[J].Journal of the Geological Society,1977,133(3):191-213.
[33]Faulkner D R,Jackson C A L,Lunn R J,et al.A review of recent developments concerning the structure,mechanics and fluid flow properties of fault zones[J].Journal of Structural Geology,2010,32:1557-1575.
[34]Chester F M,Logan J M.Implications for mechanical properties of brittle faults from observations of the Punchbowl fault zone,California[J].Pure and Applied Geophysics,1986,124:79-106.
[35]Faulkner D R,Rutter E H.The effect of temperature,the nature of the pore fluid,and subyield differential stress on the permeability of phyllosilicate-rich fault gouge[J].Journal of Geophysical Research——Solid Earth,2003,108(B5).
[36]王焕,李海兵,裴军令,等.汶川地震断裂带结构、岩性特征及其与地震活动的关系[J].第四纪研究,2010,30(4):768-778.Wang Huan,Li Haibing,Pei Junling,et al.Structural and lithologic characteristics of the Wenchuan earthquake fault zone and its relationship with the seismic activity[J].Quaternary Sciences,2010,30(4):768-778(in Chinese with English abstract).
[37]Togo T,Shimamoto T,Ma S L,et al.Internal structure of Longmenshan fault zone at Hongkou outcrop,Sichuan,China,that caused the2008Wenchuan earthquake[J].Earthquake Science,2011,24:249-265,dio:10.1007/s11589-011-0789-z.
[38]Lin A M,Maruyama T,Kobayashi K.Tectonic implications of damage zone-related fault-fracture networks revealed in drill core through the Nojima fault,Japan[J].Tectonophysics,2007,443:16-173.
[39]Sibson R H.Thickness of the seismic slip zone[J].Bulletin of the Seismological Society of America,2003,93(3):1169-1178.
[40]Kuo L W,Song S R,Yeh E C,et al.Clay mineral anomalies in the fault zone of Chelungpu Fault,Taiwan,and its implication[J].Geophysical Research Letters,2009,36(L18306):doi:10.1029/2009GL039269.
[41]Kuo L W,Song S R,Huang L,et al.Temperature estimates of coseismic heating in clay-rich fault gouges,the Chelungpu fault zones,Taiwan[J].Tectonophysics,2011,502(3-4):315-327.
[42]Kano Y,Mori J,Fujio R,et al.Heat signature on the Chelungpu fault associated with the1999Chi-Chi,Taiwan earthquake[J].Geophysical Research Letters,2006,33(L14306):doi:10.1029/2006GL026733.
[43]Li H B,Xu Z Q,Si J L,et al.Characteristics of the fault-related rocks,fault zone structures and the principal slip zone of the Wenchuan earthquake in WFSD drilling cores American Geophysical Union,Fall Annual Meeting,San Francisco,2010,T53E-02,Dec.13-17.
[44]Hirono T,Ikehara M,Otsuki K,et al.Evidence of frictional melting from disk-shaped black material,discovered within the Taiwan Chelungpu fault system[J].Geophysical Research Letters,2006,33(L19311):doi:10.1029/2006GL027329.
[45]Hirono T,Fujimoto K,Yokoyama T,et al.Clay mineral reactions caused by frictional heating during an earthquake:An example from the Taiwan Chelungpu fault[J].Geophysical Research Letters,2008,35(L16303):doi:10.1029/2008GL034476.
[46]Tanikawa W,Mishima T,Hirono T,et al.High magnetic susceptibility produced by thermal decomposition of core samples from the Chelungpu fault in Taiwan[J].Earth and Planetary Science Letters,2008,272(1-2):372-381.
[47]裴军令,李海兵,孙知明,等.汶川地震断裂带断层滑移作用—来自高磁化率断层岩的信息[J].第四纪研究,2010,30(4):750-758.Pei Junling,Li Haibing,Sun Zhiming,et al.Fault slip in the Wenchuan earthquake fault zone——information from fault rocks with higher magnetic susceptibility[J].Quaternary Sciences,2010,30(4):759-767(in Chinese with English abstract).
[48]Si J L,Li H B,Song S R,et al.Clay mineral anomalies in WFSD drilling core and surface fault rocks and their significnces.American Geophysical Union,Fall Annual Meeting.San Francisco,T51B-2044,Dec.13–17,2010.
[49]Lin A M.Seismic slip recorded by fluidized ultracataclastic veins formed in a coseismic shear zone during the2008Mw7.9Wenchuan earthquake[J].Geology,2011,39:547-550,doi:10.1130/G32065.1.
[50]Togo T,Shimamoto T,Ma S L,et al.Internal structure of Longmenshan fault zone at Hongkou outcrop,Sichuan,China,that caused the2008Wenchuan earthquake[J].Earthquake Science,2011,24:249-265.
[51]林传勇,史兰斌,刘行松,等.断层泥在基岩区断层新活动研究中的意义[J].中国地震,1995,11(1):26-32.Lin Chuanyong,Shi Lanbin,Liu Xingsong,et al.Significance of fault gouge in the study of recent activity of fault in bedrock area[J].Earthquake research in China,1995,11(1):26-32(in Chinese with English abstract).
[52]Sibson R H.Generation of pseudotachylyte by ancient seismic faulting[J].Geophysical Journal of Royal Astronomical Society,1975,43:775-794.
[53]Clark M K,House M A,Royden L H,et al.Late Cenozoic uplift of southeastern Tibet[J].Geology,2005,33,525-529.
[54]Godard V,Pik R,LavéJ,et al.Late Cenozoic evolution of the central Longmen Shan,eastern Tibet:Insight from(U-Th)/He thermochronmetry[J].Tectonics,2009,28,TC5009.
[55]Kirby E,Reiners P W,Krol M A,et al.Late Cenozoic evolution of the eastern margin of the Tibetan Plateau:Inferences from40Ar/39Ar and(U-Th)/He thermochronology[J].Tectonics,2002,21,TC1246.
[56]Ouimet W,Whipple K,Royden L,et al.Regional incision of the eastern margin of the Tibetan Plateau[J].Lithosphere,2010,2,50-63.
[57]Wang E Q,Kirby E,Furlong K P,et al.Two-phase growth of high topography in eastern Tibet during the Cenozoic[J].Nature Geoscience,2012,doi:10.1038/NGEO1538.