滇西南地震观测与分析研究
|
摘要
位于中国西南的川滇地区在印度板块和欧业板块持续碰撞的动力学背景下,第四纪以来构造活动强烈,并且形成了由川滇外弧带和滇西内弧带构成的独特的双弧型旋扭活动构造体系。其中滇西内弧带是我国构造格局最复杂,地震活动性最高的区域之一。
基于地表的调查资料难以判断活动断裂的深部产状和延伸范围,中国地质科学院地质力学研究所于2010年3月至2011年3月在瑞丽及其周边部署了由24个短周期地震台站组成的台阵,目的是通过所观测到的大量微地震的空间分布来研究区域上断裂带的空间展布、相互关系以及地震活动性。通过地震定位与误差分析等常规的处理,得到了一年以来瑞丽地区共计527个地震事件的震源参数。在分析这些地震事件的水平展布与深部剖面分布后,认为瑞丽地区在近期总体上地震活动性不强,就当地的主要活动断裂而言畹町断裂的地震活动性要强于龙陵——瑞丽断裂,而且在瑞丽市的东南方向还存在‘个地震密度相对较高的近南北向的次级构造带。
除此以外我们的短周期地震台阵还记录了台阵北北西方向约60km处的2011年3月10日盈江5.9级地震的前震和余震信息,在分别利用Hypo71绝对定位和HypoDD双差分相对定位方法对所记录到的地震进行了高精度定位后。地震时空分布显示,盈江地区的地震活动自2010年12月起开始逐渐增强；2011年3月10日Ms5.9级主震前存在3次密集震群、且有多次4级以上前震和余震发生;Ms5.9级主震及4级以上的前震均发生在苏典断裂与大盈江断裂的交汇处。从地震垂直分布上看,在北东走向大盈江断裂与苏典断裂交汇处的前震和余震呈向南东倾的带状分布,表明大盈江断裂在本次主震发生区域的倾向为南东。虽然地震的震源机制解显示大盈江断裂为主震断裂,但是由于多数小于4级的前震和余震主要沿近南北向苏典断裂呈带状分布,据此可以推测苏典断裂可能是2011年盈江地震及其前震和余震的控震构造。那么,控制前震和余震发生的控震构造与主震断裂归属走向不同的断裂。为深入分析两者差异的本质原因,这里对2008年至2010年间区域大地震活动与2011年盈江地震的关联性进行了库仑应力变化分析,首先,这些大地震均使沿苏典断裂断裂5km左右深度的库仑应力增强,这应该是盈江地震前震和余震多沿苏典断裂分布的根本原因。在大盈江断裂与苏典断裂交汇处,这些大地震(尤其是在苏典断裂发生的6级地震)对盈江地震震源机制两个破裂而中沿大盈江断裂方向的破裂面在10km深度以上的库仑应力都有增强作用,而对沿另一个与苏典断裂走向接近的破裂面的库仑应力的增强作用较弱,这解释了为什么虽然苏典断裂比大盈江断裂具有更强的地震活动性,但大盈江断裂仍然是盈江地震的主震断裂的原因。
Controlled by geodynamic background of India-Eurasia collision, Sichuan and Yunnan area in southwestern China develops intensive tectonic activities, and develops double arc rotational tectonic system which comprised by Sichuan Yunnan outer arc zone and western Yunnan inner arc zone. Western Yunnan inner arc zone is one of the area which has the most complex tectonic framework and strongest seismic activity.
For the surface geology investigation is hard to decide the attitude of active faults in depth, a portable seismic network with dense short-period seismeters deployed by Inst. Geomechanics, CAGS in Ruili during2010.3-2011.3, and the purpose is research the spatial distribution, correlations and seismic activity of major active faults in the area by microearthquake data. We got527microearthquakes and their focal parameters in Ruili area through generic processing such as earthquake location and error analysis. By analysis of the spatial distribution of these microearthquakes, we suggest that the seismic activity in Ruili area is not strong recently, and the activity of Wanding fault is higher than Longling-Ruili fault. Besides, there shows a high seismic activity N-S tectonic belt, southeast of Ruili.
Fortunately, our seismic network recorded the Ms5.9earthquake occurred at the Yingjiang town on March10th,2011.-60km far away from Ruili, but also recorded the foreshocks and aftershocks. All the earthquakes were located firstly with the HYPO71and then relocated by HYPODD. The results show that seismic activity in the Yingjiang area became higher since December,2010; then three earthquake swarms and several foreshocks stronger than Ml4.0occurred before the mainshock; Both the mainshock and all the foreshocks stronger than Ml4.0occurred at/around the intersection of the NNW-SSE Sudian Fault and the NE-SW Dayingjiang Fault. Vertically, foreshocks and aftershocks aligned in a SE-dipped belt around the intersection of the two faults, indicates that the Dayingjiang fault dips SE at/around the mainshock. Although Focal mechanism of the main shock indicated that the Dayingjiang Fault is the seismogenic fault of the mainshock, however, most foreshocks and aftershocks distribute as a belt along the NNW-SSE Sudian Fault, indicating that the seismicity of Yingjiang during2010-2011is mainly controlled by the Sudian Fault. In order to understand why mean that the seismogenic fault of the mainshock is different with the regional active seismogenic fault, we analyzed the relationship between regional strong shocks happened in2008-2010and the2011Yingjiang earthquake by Coulomb Stress analysis. At first, the strong shocks increased coulomb stress in a plane parallel to the Sudian fault in a large area along/close to the Sudian fault at the depth of-5km, which can interpret why the foreshocks and aftershocks of the2011Yingjiang earthquake distributed along the Sudian Fault. The three strong shocks, especially the Ms6.1earthquake occurred at Sudian Fault, increased coulomb stress at the intersection of the Sudian Fault and the Dayingjiang Fault, at both the possible fault planes of the2011-Yingjiang-earthquake focal mechanism down to10km deep, however, the increase of coulomb stress along the plane parallel to the Dayingjiang fault is obviously higher than the other plane which is close to the strike of the Sudian Fault, which can interpret that although the seismic activity of the Sudian Fault is stronger than the Dayingjiang Fault, the Dayingjiang Fault is the seismogenic fault of the mainshock
基于地表的调查资料难以判断活动断裂的深部产状和延伸范围,中国地质科学院地质力学研究所于2010年3月至2011年3月在瑞丽及其周边部署了由24个短周期地震台站组成的台阵,目的是通过所观测到的大量微地震的空间分布来研究区域上断裂带的空间展布、相互关系以及地震活动性。通过地震定位与误差分析等常规的处理,得到了一年以来瑞丽地区共计527个地震事件的震源参数。在分析这些地震事件的水平展布与深部剖面分布后,认为瑞丽地区在近期总体上地震活动性不强,就当地的主要活动断裂而言畹町断裂的地震活动性要强于龙陵——瑞丽断裂,而且在瑞丽市的东南方向还存在‘个地震密度相对较高的近南北向的次级构造带。
除此以外我们的短周期地震台阵还记录了台阵北北西方向约60km处的2011年3月10日盈江5.9级地震的前震和余震信息,在分别利用Hypo71绝对定位和HypoDD双差分相对定位方法对所记录到的地震进行了高精度定位后。地震时空分布显示,盈江地区的地震活动自2010年12月起开始逐渐增强；2011年3月10日Ms5.9级主震前存在3次密集震群、且有多次4级以上前震和余震发生;Ms5.9级主震及4级以上的前震均发生在苏典断裂与大盈江断裂的交汇处。从地震垂直分布上看,在北东走向大盈江断裂与苏典断裂交汇处的前震和余震呈向南东倾的带状分布,表明大盈江断裂在本次主震发生区域的倾向为南东。虽然地震的震源机制解显示大盈江断裂为主震断裂,但是由于多数小于4级的前震和余震主要沿近南北向苏典断裂呈带状分布,据此可以推测苏典断裂可能是2011年盈江地震及其前震和余震的控震构造。那么,控制前震和余震发生的控震构造与主震断裂归属走向不同的断裂。为深入分析两者差异的本质原因,这里对2008年至2010年间区域大地震活动与2011年盈江地震的关联性进行了库仑应力变化分析,首先,这些大地震均使沿苏典断裂断裂5km左右深度的库仑应力增强,这应该是盈江地震前震和余震多沿苏典断裂分布的根本原因。在大盈江断裂与苏典断裂交汇处,这些大地震(尤其是在苏典断裂发生的6级地震)对盈江地震震源机制两个破裂而中沿大盈江断裂方向的破裂面在10km深度以上的库仑应力都有增强作用,而对沿另一个与苏典断裂走向接近的破裂面的库仑应力的增强作用较弱,这解释了为什么虽然苏典断裂比大盈江断裂具有更强的地震活动性,但大盈江断裂仍然是盈江地震的主震断裂的原因。
Controlled by geodynamic background of India-Eurasia collision, Sichuan and Yunnan area in southwestern China develops intensive tectonic activities, and develops double arc rotational tectonic system which comprised by Sichuan Yunnan outer arc zone and western Yunnan inner arc zone. Western Yunnan inner arc zone is one of the area which has the most complex tectonic framework and strongest seismic activity.
For the surface geology investigation is hard to decide the attitude of active faults in depth, a portable seismic network with dense short-period seismeters deployed by Inst. Geomechanics, CAGS in Ruili during2010.3-2011.3, and the purpose is research the spatial distribution, correlations and seismic activity of major active faults in the area by microearthquake data. We got527microearthquakes and their focal parameters in Ruili area through generic processing such as earthquake location and error analysis. By analysis of the spatial distribution of these microearthquakes, we suggest that the seismic activity in Ruili area is not strong recently, and the activity of Wanding fault is higher than Longling-Ruili fault. Besides, there shows a high seismic activity N-S tectonic belt, southeast of Ruili.
Fortunately, our seismic network recorded the Ms5.9earthquake occurred at the Yingjiang town on March10th,2011.-60km far away from Ruili, but also recorded the foreshocks and aftershocks. All the earthquakes were located firstly with the HYPO71and then relocated by HYPODD. The results show that seismic activity in the Yingjiang area became higher since December,2010; then three earthquake swarms and several foreshocks stronger than Ml4.0occurred before the mainshock; Both the mainshock and all the foreshocks stronger than Ml4.0occurred at/around the intersection of the NNW-SSE Sudian Fault and the NE-SW Dayingjiang Fault. Vertically, foreshocks and aftershocks aligned in a SE-dipped belt around the intersection of the two faults, indicates that the Dayingjiang fault dips SE at/around the mainshock. Although Focal mechanism of the main shock indicated that the Dayingjiang Fault is the seismogenic fault of the mainshock, however, most foreshocks and aftershocks distribute as a belt along the NNW-SSE Sudian Fault, indicating that the seismicity of Yingjiang during2010-2011is mainly controlled by the Sudian Fault. In order to understand why mean that the seismogenic fault of the mainshock is different with the regional active seismogenic fault, we analyzed the relationship between regional strong shocks happened in2008-2010and the2011Yingjiang earthquake by Coulomb Stress analysis. At first, the strong shocks increased coulomb stress in a plane parallel to the Sudian fault in a large area along/close to the Sudian fault at the depth of-5km, which can interpret why the foreshocks and aftershocks of the2011Yingjiang earthquake distributed along the Sudian Fault. The three strong shocks, especially the Ms6.1earthquake occurred at Sudian Fault, increased coulomb stress at the intersection of the Sudian Fault and the Dayingjiang Fault, at both the possible fault planes of the2011-Yingjiang-earthquake focal mechanism down to10km deep, however, the increase of coulomb stress along the plane parallel to the Dayingjiang fault is obviously higher than the other plane which is close to the strike of the Sudian Fault, which can interpret that although the seismic activity of the Sudian Fault is stronger than the Dayingjiang Fault, the Dayingjiang Fault is the seismogenic fault of the mainshock
引文
ACHARYA, H.K., FERGUSON, J.F., and ISAAC, V.,1979, Microearthquake surveys in the Central and Northern Philippines:Bulletin of the Seismological Society of America, v.69, p.1889-1902.
Aki, K., and Richards, P.G.,1980, Quantitative Seismology:New York, W.H. Freeman.
Allen, R.V.,1978, Automatic earthquake recognition and timing from single traces:Bulletin of the Seismological Society of America, v.68, p.1521-1532.
Allen, R.V.,1982, Automatic phase pickers:Their present use and future prospects:Bulletin of the Seismological Society of America, v.72, p.225-242.
An, M., Feng, M., and Long, C.,2010, Deep ruptures around the hypocenter of the 12 May 2008 Wenchuan Earthquake deduced from aftershock observations:Tectonophysics, v.491, p. 96-104.
Anderson, K.R.,1982, Robust earthquake location using M-estimates:Physics of the Earth and Planetary Interiors, v.30, p.119-130.
Astiz, L., Shearer, P.M., and Agnew, D.C.,2000, Precise relocations and stress change calculations for the Upland earthquake sequence in southern California:Journal of Geophysical Research, v. 105, p.2937-2953.
Bai, and D.,2003, Deep structure of the Longling-Ruili fault underneath Ruili basin near the eastern Himalayan syntaxis:insights from magnetotelluric imaging:Tectonophysics, v.364, p. 135-146.
Bai, D., and Meju, M.A.,2003, Deep structure of the Longling-Ruili fault underneath Ruili basin near the eastern Himalayan syntaxis:Tectonophysics, p.135-146.
Bird, P.,2003, An updated digital model of plate boundaries:Geochemistry Geophysics Geosystems, v. 4, p.1-52.
Bodin, P., and Horton, S.,2004, Source parameters and tectonic implications of aftershocks of the Mw 7.6 Bhuj earthquake of 26 January 2001:Bulletin of the Seismological Society of America, v. 94, p.818-827.
Bormann, P.,2002, New Manual of Seismological Observatory Practice (NMSOP):Potsdam, GeoForschungsZentrum.
Buland, R., and Chapman, C.H.,1983, The computation of seismic travel times:Bulletin of the Seismological Society of America, v.73, p.1271-1302.
Chave, A.D., Thomson, D.J., and Ander, M.E.,1987, On the robust estimation of power spectra, coherences, and transfer functions:Journal of Geophysical Research, v.92, p.633-648.
Coffin, M.F., Gahagan, L.M., and and Lawver, L.A.,1998, Present-day plate boundary digital data compilation, University of Texas Institute for Geophysics Technical Report, p.5.
Douglas, A.,1967, Joint hypocenter determination:Nature, v.215, p.47-48.
Douglas, A., Bowers, D., and Young, J.B.,1997, On the onset of P seismograms:Geophys. J. Int., v.129, p.681-690.
Feng, M., An, M., Zhao, L., and Zhang, J.,2009, Depth and region dependence of b-value for micro-aftershocks of the May 12th,2008 Wenchuan earthquake and its tectonic implications: Earthquake Science, v.22, p.589-594.
Fischer, T., and Horalek, J.,2000, Refined Locations of The Swarm Earthquakes In The Novy Kostel Focal Zone and Spatial Distribution of The January 1997 Swarm In Western Bohemia, Czech Republic:Studia Geophysica et Geodaetica, v.44, p.210-226.
Fitch, T.J.,1975, Compressional velocity in source regions of deep earthquakes:An application of the master earthquake technique:Earth and Planetary Science Letters, v.26, p.156-166.
Frechet, J.,1985, Sismogenese et doublets sismiques:Travaux Universitaires-These d'Etat, p.206.
Fremont, M.-J., and Malone, S.D.,1987, High precision relative locations of earthquakes at Mount St. Helens, Washington:Journal of Geophysical Research, v.92, p.10223-10236.
Freed, A.M.,2005, Earthquake triggering by static, dynamic, and postseismic stress transfer, Annual Review of Earth and Planetary Sciences, Volume 33, p.335-367.
Geiger, L.,1912, Probability method for the determination of earthquake epicenters from arrival time only, Bull.St.Louis.Univ, Volume 8, p.60-71.
Giardini, D., and Basham, P.,1993, The Global Seismic Hazard Assessment Program (GSHAP).
Giardini, D., Griinthal, G., Shedlock, K.M., and Zhang, P.,1999, The GSHAP Global Seismic Hazard Map: Annali Di Geofisica, v.42, p.1225-1230.
Giovambattista, R.D., and Barba, S.,1997, An estimate of hypocentre location accuracy in a large network:possible implications for tectonic studies in Italy:Geophys. J. Int., v.129, p.124-132.
Got, J.-L., Frechet, J., and Klein, F.W.,1994, Deep fault plane geometry inferred from multiplet relative relocation beneath the south flank of Kilauea:Journal of Geophysical Research, v.99, p. 15375-15386.
Gross, S., and Burgmann, R.,1998, Rate and state of background stress estimated from the aftershocks of the 1989 Loma Prieta, California, earthquake:Journal of Geophysical Research, v.103, p. 4915-4927.
Harris, R.A.,1998, Introduction to special section:stress triggers, stress shadows, and implications for seismic hazard:Journal of Geophysical Research, v.103, p.24347-24358.
Harris, R.A.,2000, Earthquake stress triggers, stress shadows, and seismic hazard:Current Science, v. 79, p.1215-1225.
Harris, R.A., and Simpson, B.W.,1992, Changes in static stress on southern California faults after the 1992 Landers earthquake, Nature, Volume 360, p.251-254.
Heppe, K., Helmcke, D., and Wemmer, K.,2007, The Lancang River Zone of southwestern Yunnan, China:A questionable location for the active continental margin of Paleotethys:Journal of Asian Earth Sciences, v.30, p.706-720.
Huang, J.,2002, Lithospheric structure and its relationship to seismic and volcanic activity in southwest China:Journal of Geophysical Research, v.107, p.2255.
Jaeger, J.C., and Cook, N.G.W.,1969, Fundamentals of Rock Mechanics:London, Methuen and Co.
Joswig, M.,1990, Pattern recognition for earthquake detection:Bulletin of the Seismological Society of America, v.80, p.170-186.
Joswig, M.,1993, Single-trace detection and array-wide coincidence association of local earthquakes and explosions:Computers and Geosciences, v.19, p.207-221.
Kiimpel, H.-J.,1991, Poroelasticity:parameters reviewed:Geophys. J. Int., v.105, p.783-799.
Kagan, Y.Y.,1994, Incremental Stress and Earthquakes:Geophys. J. Int,v.117, p.345-364.
Kagan, Y.Y., and Jackson, D.D.,1998, Spatial aftershock distribution:Effect of normal stress:Journal of Geophysical Research, v.103, p.24453-24467.
Karakostas, V.G.,2003, The 2001 Skyros, Northern Aegean, Greece, earthquake sequence:off-fault aftershocks, tectonic implications, and seismicity triggering:Geophysical Research Letters, v. 30, p.1-12.
Kennet, B.L.N., and Engdahl, E.R.,1991, IASPEI 1991 seismological tables:Terra Nova, v.3, p.122.
King, G.C.P., Stein, R.S., and Lin, J.,1994, static stress changes and the triggering of earthquakes: Bulletin of the Seismological Society of America, v.84, p.935-953.
Lacassin, R., Replumaz, A., and Lelou, P.H.,1998, Hairpin river loops and slip-sense inversion on southeast Asian strike-slip faults:Geology, v.26, p.703-706.
Lawson, C.L., and Hanson, R.J.,1974, Solving Least Squares Problems:New Jersey, Prentice-Hall.
Lee, W.H.K., and Lahr, J.C.,1975, HYPO71:A computer program for determining hypocenter magnitude, and first motion pattern of local earthquakes:California, USGS.
Lei, J., Xie, F., Mishra, O.P., Lu, Y., Zhang, G., and Li, Y.,2012, The 2011 Yingjiang, China, earthquake:a volcano-related fluid-driven earthquake?:Bulletin of the Seismological Society of America, v. 102, p.417-425.
Li, C., Vanderhilst, R., Meltzer, A., and Engdahl, E.,2008a, Subduction of the Indian lithosphere beneath the Tibetan Plateau and Burma:Earth and Planetary Science Letters, v.274, p. 157-168.
Li, C., Vanderhilst, R., and Toksoz, M.,2006, Constraining P-wave velocity variations in the upper mantle beneath Southeast Asia:Physics of The Earth and Planetary Interiors, v.154, p. 180-195.
Li, Y., Wu, Q., Zhang, R., Tian, X., and Zeng, R.,2008b, The crust and upper mantle structure beneath Yunnan from joint inversion of receiver functions and Rayleigh wave dispersion data:Physics of The Earth and Planetary Interiors, v.170, p.134-146.
Liang, C.,2004, Tomographic inversion of Pn travel times in China:Journal of Geophysical Research, v. 109, p. B11304.
Lienert, B., and Havskov, J.,1995, A computer program for locating earthquakes both locally and globally:Seismological Research Letters, v.66, p.26-36.
Lomax, A., Virieux, J., Volant, P., and Berge-Thierry, C.,2000, Probabilistic Earthquake Location in 3D and Layered Models:Advances in Seismic Event Location Modern Approaches in Geophysics, v. 18, p.101-134.
Lomax, A., Zollo, A., Capuano, P., and Virieuxl, J.,2001, Precise, absolute earthquake location under Somma-Vesuvius volcano using a new three-dimensional velocity model:Geophys. J. Int., v. 146, p.313-331.
Menke, W.,1999, Using waveform similarity to constrain earthquake locations:Bulletin of the Seismological Society of America, v.89, p.1143-1146.
Mogi, K.,1979, Two kinds of seismic gaps:Pure Appl. Geophys., v.117, p.1172-1186.
Morley, C.K.,2007, Variations in Late Cenozoic-Recent strike-slip and oblique-extensional geometries, within Indochina:The influence of pre-existing fabrics:Journal of Structural Geology, v.29, p. 36-58.
Mosteller, F., and Tukey, J.W.,1977, Data analysis and regression:a second course in statistics.: Massachussets, Addison-Wesley, Reading.
Muller, G.,1977, Earth-flattening approximation for body waves derived from geometric ray theory-improvements, corrections and range of applicability:J. Geophys., v.58, p.153-174.
Murdock, J.N., and Hutt, C.R.,1983, A new event detector designed for the seismic research observatories, Volume Open File Report, USGS, p.83-7851.
Nalbant, S.S., Hubert, A., and King, G.C.P.,1998, Stress coupling between earthquakes in northwest Turkey and the north Aegean Sea:Journal of Geophysical Research, v.103, p.24469-24486.
Nielsen, C., Chamot-Rooke, N., and Rangin, C,2004, From partial to full strain partitioning along the Indo-Burmese hyper-oblique subduction:Marine Geology, v.209, p.303-327.
Paige, C.C., and Saunders, M.A.,1982, LSQR:An Algorithm for Sparse Linear Equations and Sparse Least Squares:ACM Transactions on Mathematical Software, v.8, p.43-71.
Parolai, S., Trojani, L., Monachesi, G., Frapiccini, M., Cattaneo, M., and Augliera, P.,2001, Hypocenter location accuracy and seismicity distribution in the Central Apennines (Italy):Journal of Seismology, v.5, p.243-261.
Peltzer, G., and Tapponnier, P.,1988, Formation and evolution of strike-slip faults, rifts, and basins during the India-Asia Collision:An experimental approach:Journal of Geophysical Research, v. 93, p.15085-15117.
Peppin, W.A., Honjas, W., Somerville, M.R., and Vetter, U.R.,1989, Precise master-event locations of aftershocks of the 4 October 1978 Wheeler Crest earthquake sequence near Long Valley, California:Bulletin of the Seismological Society of America, v.79, p.67-76.
Poupinet, G., Ellsworth, W.L., and Frechet, J.,1984, Monitoring velocity variations in the crust using earthquake doublets:An application to the Calaveras Fault, California:Journal of Geophysical Research, v.89, p.5719-5731.
Reasenberg, P.A., and Simpson, R.W.,1992, Response of regional seismicity to the static stress change produced by the Loma Prieta earthquake:Science, v.255, p.1687-1690.
Rice, J.R.,1992, Fault Stress States, Pore Pressure Distributions, and the Weakness of the San Andreas Fault:International Geophysics, v.51, p.475-503.
Rice, J.R., and Cleary, M.P.,1976, Some basic stress diffusion solutions for fluid-saturated elastic porous media with compressible constituents:Reviews of Geophysics, v.14, p.227-241.
Roeloffs, E., and Rudnicki, J.W.,1985, Coupled deformation-diffusion effects on water-level changes due to propagating creep events:Pure Appl. Geophys., v.122, p.560-582.
Roeloffs, E.A.,1988, Fault stability changes induced beneath a reservoir with cyclic variations in water level:Journal of Geophysical Research, v.93, p.2107-2124.
Roeloffs, E.A.,1996, Poroelastic techniques in the study of earthquake-related hydrologic phenomena: Advances in Geophysics, v.37.
Ruzek, B., and Kvasnicka, M.,2001, Differential Evolution Algorithm in the Earthquake Hypocenter Location:Pure appl. Geophys., v.158, p.667-693.
Sambridge, M.S., and Kennett, B.L.N.,1986, A novel method of hypocentre location:Geophys. J. Int., v. 87, p.679-697.
Sambridge, M.S., and Kennett, B.L.N.,2001, Seismic Event Location:Nonlinear Inversion Using a Neighbourhood Algorithm:Pure appl. Geophys., v.158, p.241-257.
Schweitzer, J.,2001, HYPOSAT - An Enhanced Routine to Locate Seismic Events:Pure appl. Geophys., v.158, p.277-289.
Shedlock, K.M., Giardini, D., GriJnthal, G., and Zhang, P.,2000, The GSHAP Global Seismic Hazard Map: Seismological Research Letters, v.71, p.679-686.
Skempton, A.W.,1954, The Pore-Pressure Coefficients A and B:Geotechnique, v.4, p.143-147.
Socquet, A., and Pubellier, M.,2005, Cenozoic deformation in western Yunnan (China-Myanmar border):Journal of Asian Earth Sciences, v.24, p.495-515.
Spence, W.,1980, Relative epicenter determination using P-wave arrival-time differences:Bulletin of the Seismological Society of America, v.70, p.171-183.
Stein, R.S., King, G.C.P., and Lin, J.,1992, Change in Failure Stress on the Southern San Andreas Fault System Caused by the 1992 Magnitude= 7.4 Landers Earthquake:Science, v.258, p.1328-1332.
Stein, S., and Wysession, M.,1991, An Introduction to Seismology, Earthquakes and Earth Structures.: Evanston, Northwesten Univercity, USA.
Tao, W., and Shen, Z.,2008, Heat flow distribution in Chinese continent and its adjacent areas: Progress in Natural Science, v.18, p.843-849.
Troise, C., De Natale, G., Pingue, F., and Petrazzuoli, S.M.,1998, Evidence for static stress interaction among earthquakes in the south-central Apennines:Geophys. J. Int., v.134, p.809-817.
Waldhauser, F.,2001, HYPODD-A program to compute double-difference hypocenter locations: California, U. S. Geologic Survey.
Waldhauser, F., and Ellsworth, W.L.,2000, A double-difference earthquake location algorithm:method and application to the northern Hayward fault, California:Bulletin of the Seismological Society of America, v.90, p.1353-1368.
Wang, and C.,2004, Crustal structure in Tengchong Volcano-Geothermal Area, western Yunnan, China: Tectonophysics, v.380, p.69-87.
Wang, C.-Y.,2003, Three-dimensional velocity structure of crust and upper mantle in southwestern China and its tectonic implications: Journal of Geophysical Research, v.108, p.2442.
Wang, E., and Burchfiel, B.C.,1997, Interpretation of Cenozoic Tectonics in the Right-Lateral Accommodation Zone Between the Ailao Shan Shear Zone and the Eastern Himalayan Syntaxis:International Geology Review, v.39, p.191-219.
Wang, Y, Fan, W., Zhang, Y., Peng, T., Chen, X., and Xu, Y.,2006, Kinematics and 40Ar/39Ar geochronology of the Gaoligong and Chongshan shear systems, western Yunnan, China: Implications for early Oligocene tectonic extrusion of SE Asia:Tectonophysics, v.418, p. 235-254.
Wells, D.L., and Coppersmith, K.J.,1994, New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement:Bulletin of the Seismological Society of America, v.84, p.974-1002.
Wiechert, E., and Zoeppritz, K.,1907, Ueber erdbebenwellen:Nachrichten von der Gesellschaft der Wissenschaften zu Gottingen, Mathematisch-Physikalische Klasse, p.413-529.
Xiong, X., Shan, B., Zheng, Y, and Wang, R.,2010, Stress transfer and its implication for earthquake hazard on the Kunlun Fault, Tibet:Tectonophysics, v.482, p.216-225.
Xu, L., Rondenay, S., and van der Hilst, R.D.,2007, Structure of the crust beneath the southeastern Tibetan Plateau from teleseismic receiver functions:Physics of The Earth and Planetary Interiors, v.165, p.176-193.
Yang, Z., Chen, Y., and Zhang, H.,2002, Relocation and seismogenic structure of the 1998 Zhangbei-Shangyi earthquake sequence:Acta Seismologica Sinica, v.15, p.383-394.
Zhang, X., and Wang, Y.,2009, Crustal and upper mantle velocity structure in Yunnan, Southwest China: Tectonophysics, v.471, p.171-185.
Zhao, D.,2007, Seismic images under 60 hotspots:Search for mantle plumes:Gondwana Research, v. 12, p.335-355.
Zhao, D.,2009, Multiscale seismic tomography and mantle dynamics:Gondwana Research, v.15, p. 297-323.
Zhou, H., Liu, H.-L., and Kanamori, H.,1983, Source processes of large earthquakes along the Xianshuihe fault in southwestern China:Bulletin of the Seismological Society of America, v.73, p.537-551.
万永革,吴忠良,周公威,and黄静,2000,几次复杂地震中不同破裂事件之间的“应力触发”问题：地震学报,v.22,p.568-576.
毛玉平,韩新民,and谷一山,2003,云南地区强震(M≥6)研究：昆明,云南科技出版社.
王刚,万景林,and王二七,2006,高黎贡山脉南部的晚新生代构造—重力垮塌及其成因：地质学报,v.80,p.1262-1273.
王晋南,王洋龙,安晓文,杨向东,and常祖峰,2006,1976年龙陵地震区断裂活动性研究：地震研究,v.29,p.366-372.
王阎昭,王恩宁,沈正康,王敏,甘卫军,乔学军,孟国杰,李铁明,陶玮,杨永林,程佳,and李鹏,2008,基于GP5资料约束反演川滇地区主要断裂现今活动速率：中国科学(D辑),v.38,p.582-597.
付虹,黄浩,李丽,and赵小艳,2011,2011年3月10日云南盈江5.8级地震序列研究：地震研究v.34,p.414-419.
田玥,and陈晓非,2002,地震定位研究综述：地球物理学进展,v.17,p.147-155.
安晓文,常祖峰,and石静芳,2009,大盈江断裂西南段晚第四纪活动研究：地震研究,v.32,p.193-197.
朱成男,1979,龙陵地震地质背景：地震研究,p.53-64.
李四光,1973,地质力学概论：北京,科学出版社.
李四光,1974,旋扭构造：北京,科学出版社.
李四光,1979,地质力学方法：北京,科学出版社.
杜义,张效亮,黄学猛,杜宇本,and谢富仁,2012,龙陵-瑞丽断裂北段晚第四纪活动性特征及强震复发间隔：震灾防御技术,v.7,p.215-226.
周立功,1983,微震台网在地质工作中的应用：中国地质,p.21-26.
房立华,吴建平,张天中,黄静,王长在,and杨婷,2011,2011年云南盈江Ms5.8地震及其余震序列重定位：地震学报,v.33,p.262-267.
姚鑫,张加桂,张永双,杨波,and余凯,2011,2011年3月10日盈江5.8级地震诱发砂土液化灾害特征研究：工程地质学报,v.2,p.152-161.
胡鸿翔,林中洋,边银菊,王椿镛,and朱良保,1996,滇西地区壳幔慢过渡带性质的研究：地震学报,v.18,p.444-450.
胡鸿翔,陆涵行,and 王椿镛,1993,滇西地区地壳浅部基底速度细结构的研究：中国地震,v.9,p.356-364.
胡鸿翔,陆涵行,王椿铺,何正勤,and朱良保,1986,滇西地区地壳结构的爆破地震研究：地球物理学报,v.29,p.133-144.
徐纪人,赵志新,and石川有三,2008,中国大陆地壳应力场与构造运动区域特征研究：地球物理学报,v.51,p.770-781.
常祖峰,安晓文,and张艳凤,2012,畹町断裂晚第四纪活动与水系构造变形：地震地质,v.34,p.228-239.
常祖峰,陈刚,and余建强,2011,大盈江断裂晚更新世以来活动的地质证据：地震地质,v.33,p.877-888.
傅竹武,王苏,刘建华,and胥颐,2007a,利用接收函数方法研究瑞丽—龙陵断裂两侧S波速度结构：地震研究,v.30,p.223-228.
傅竹武,刘建华,胥颐,文丽敏,续外芬,and马红虎,2007b,利用接收函数方法研究大盈江断裂两侧S波速度结构：云南大学学报,v.29,p.607-612.
傅淑芳,and刘宝诚,1991,地震学教程：北京,地震出版社,447-480 p.
樊春,and王二七,2004,滇西高黎贡山南段左行剪切构造形迹的发现及其大地构造意义：自然科学进展,v.14,p.1189-1193.
虢顺民,向宏发,周瑞琦,徐锡伟,董兴权,and张晚霞,1999,滇西南龙陵—澜沧断裂带——大陆地壳上一条新生的破裂带：科学通报,v.44,p.2118-2121.
虢顺民,向宏发,徐锡伟,张晚霞,周瑞琦,and 董兴权,2000,滇西南龙陵—澜沧第四纪新生断裂带特征和形成机制研究：地震地质,v.22,p.277-284.
冯梅,安美健,王小凤,and马寅生,2007,青海狮子沟油田天然微地震活动及其地质意义：地质力学学报,v.13,p.173-178.
吴中海,李贵书,毛晓长,尹福光,翟刚毅,and张虎,2013,泛业铁路云南大理至瑞丽沿线基础地质与主要工程地质问题：北京,地质出版社.
吴中海,赵希涛,范桃园,叶培盛,仝亚博,and杨振宇,2012,泛亚铁路滇西大理至瑞丽沿线主要活动断裂与地震地质特征：地质通报,v.31,p.191-217.
孙泽轩,2000,盈江盆地盖层氧化带发育特征及其与铀矿化的关系：铀矿地质,v.16,p.79-84.
张小涛,吕坚,and 马广庆,2008,双差地震定位法在邯郸—邢台地区地震精确定位中的初步应用：地震研究,v.31,p.37-41.
张中杰,白志明,王椿镛,吕庆田,滕吉文,李继亮,孙善学,and王新征,2005,冈瓦纳型和扬子型地块地壳结构：以滇西孟连—马龙宽角反射剖面为例：中国科学D辑,v.34,p.387-392.
张四昌,刁桂苓,王绍晋,and龙晓帆,1994,1976年龙陵震群序列的破裂特征：中国地震,v.10,p.152-159.
张四昌,and徐杰,1978,1976年龙陵地震地震地质特征的探讨：地震研究,p.44-54.
张永北,1999,龙陵—瑞丽走滑体系中段自相似结构与热液成矿定位：地质学报,v.73,p.334-341.
杨中书,and曾文敬,2007,利用双差法对2005年江西九江—瑞昌5.7级地震序列重新定位：地震地磁观测与研究,v.28,p.25-31.
杨晶琼,杨周胜,and刘丽芳,2010a,2008年盈江5.9级地震序列震源参数研究：地震研究,v.33,p.308-312.
杨晶琼,杨周胜,刘丽芳,苏有锦,and张森,2010b,2008年盈江5.9级地震序列震源参数研究：地震研究,v.33,p.308-312.
杨智娴,陈运泰,郑月军,and于湘伟,2003,双差地震定位法在我国中西部地区地震精确定位中的应用：中国科学(D辑),v.33,p.129-134.
许忠淮,2001,东亚地区现今构造应力图的编制：地震学报,v.23,p.492-501.
许忠淮,汪素云,黄雨蕊,and高阿甲,1989,山大量的地震资料推断的我国大陆构造应力场：地球物理学报,v.32,p.636-647.
谢韬,林仕良,李富,丛峰,李再会,and邹光富,2011,龙陵—瑞丽断裂潞西段的发育特征及意义大地构造与成矿学,v.35,p.216-220.
郑钰,and杨建思,2008,双差算法的剖析及参数对定位的影响：地震地磁观测与研究,v.29,p.85-93.
钱晓东,苏有锦,付虹,and李琼,2011,2011年云南盈江5.8级地震及震前短临跟踪预测：地震研究,34,p.403-413.
阚荣举,王绍晋,and刘祖荫,1979,龙陵地震序列的震源机制特征,p.10-21.
阚荣举,and彭万里,1980,西南地区应力场变动与强震活动秩序及实验研究：地震研究,v.3,p.181-192.
陈立德,and赵维城,1979,1976年龙陵地震：北京,地震出版社.
陈顒,and黄庭芳,2001,岩石物理学：北京,北京大学出版社.
马瑾,1987,构造物理学概论：北京,地震出版社.
黄学猛,杜义,舒赛兵,and谢富仁,2010,龙陵—瑞丽断裂(南支)北段晚第四纪活动性特征：地震地质,v.32,p.222-232.
黄崐,万建平,and黄莺,1987,1976年龙陵地区地震前后垂直形变的演变过程：地震研究,v.10,p.671-680.
Aki, K., and Richards, P.G.,1980, Quantitative Seismology:New York, W.H. Freeman.
Allen, R.V.,1978, Automatic earthquake recognition and timing from single traces:Bulletin of the Seismological Society of America, v.68, p.1521-1532.
Allen, R.V.,1982, Automatic phase pickers:Their present use and future prospects:Bulletin of the Seismological Society of America, v.72, p.225-242.
An, M., Feng, M., and Long, C.,2010, Deep ruptures around the hypocenter of the 12 May 2008 Wenchuan Earthquake deduced from aftershock observations:Tectonophysics, v.491, p. 96-104.
Anderson, K.R.,1982, Robust earthquake location using M-estimates:Physics of the Earth and Planetary Interiors, v.30, p.119-130.
Astiz, L., Shearer, P.M., and Agnew, D.C.,2000, Precise relocations and stress change calculations for the Upland earthquake sequence in southern California:Journal of Geophysical Research, v. 105, p.2937-2953.
Bai, and D.,2003, Deep structure of the Longling-Ruili fault underneath Ruili basin near the eastern Himalayan syntaxis:insights from magnetotelluric imaging:Tectonophysics, v.364, p. 135-146.
Bai, D., and Meju, M.A.,2003, Deep structure of the Longling-Ruili fault underneath Ruili basin near the eastern Himalayan syntaxis:Tectonophysics, p.135-146.
Bird, P.,2003, An updated digital model of plate boundaries:Geochemistry Geophysics Geosystems, v. 4, p.1-52.
Bodin, P., and Horton, S.,2004, Source parameters and tectonic implications of aftershocks of the Mw 7.6 Bhuj earthquake of 26 January 2001:Bulletin of the Seismological Society of America, v. 94, p.818-827.
Bormann, P.,2002, New Manual of Seismological Observatory Practice (NMSOP):Potsdam, GeoForschungsZentrum.
Buland, R., and Chapman, C.H.,1983, The computation of seismic travel times:Bulletin of the Seismological Society of America, v.73, p.1271-1302.
Chave, A.D., Thomson, D.J., and Ander, M.E.,1987, On the robust estimation of power spectra, coherences, and transfer functions:Journal of Geophysical Research, v.92, p.633-648.
Coffin, M.F., Gahagan, L.M., and and Lawver, L.A.,1998, Present-day plate boundary digital data compilation, University of Texas Institute for Geophysics Technical Report, p.5.
Douglas, A.,1967, Joint hypocenter determination:Nature, v.215, p.47-48.
Douglas, A., Bowers, D., and Young, J.B.,1997, On the onset of P seismograms:Geophys. J. Int., v.129, p.681-690.
Feng, M., An, M., Zhao, L., and Zhang, J.,2009, Depth and region dependence of b-value for micro-aftershocks of the May 12th,2008 Wenchuan earthquake and its tectonic implications: Earthquake Science, v.22, p.589-594.
Fischer, T., and Horalek, J.,2000, Refined Locations of The Swarm Earthquakes In The Novy Kostel Focal Zone and Spatial Distribution of The January 1997 Swarm In Western Bohemia, Czech Republic:Studia Geophysica et Geodaetica, v.44, p.210-226.
Fitch, T.J.,1975, Compressional velocity in source regions of deep earthquakes:An application of the master earthquake technique:Earth and Planetary Science Letters, v.26, p.156-166.
Frechet, J.,1985, Sismogenese et doublets sismiques:Travaux Universitaires-These d'Etat, p.206.
Fremont, M.-J., and Malone, S.D.,1987, High precision relative locations of earthquakes at Mount St. Helens, Washington:Journal of Geophysical Research, v.92, p.10223-10236.
Freed, A.M.,2005, Earthquake triggering by static, dynamic, and postseismic stress transfer, Annual Review of Earth and Planetary Sciences, Volume 33, p.335-367.
Geiger, L.,1912, Probability method for the determination of earthquake epicenters from arrival time only, Bull.St.Louis.Univ, Volume 8, p.60-71.
Giardini, D., and Basham, P.,1993, The Global Seismic Hazard Assessment Program (GSHAP).
Giardini, D., Griinthal, G., Shedlock, K.M., and Zhang, P.,1999, The GSHAP Global Seismic Hazard Map: Annali Di Geofisica, v.42, p.1225-1230.
Giovambattista, R.D., and Barba, S.,1997, An estimate of hypocentre location accuracy in a large network:possible implications for tectonic studies in Italy:Geophys. J. Int., v.129, p.124-132.
Got, J.-L., Frechet, J., and Klein, F.W.,1994, Deep fault plane geometry inferred from multiplet relative relocation beneath the south flank of Kilauea:Journal of Geophysical Research, v.99, p. 15375-15386.
Gross, S., and Burgmann, R.,1998, Rate and state of background stress estimated from the aftershocks of the 1989 Loma Prieta, California, earthquake:Journal of Geophysical Research, v.103, p. 4915-4927.
Harris, R.A.,1998, Introduction to special section:stress triggers, stress shadows, and implications for seismic hazard:Journal of Geophysical Research, v.103, p.24347-24358.
Harris, R.A.,2000, Earthquake stress triggers, stress shadows, and seismic hazard:Current Science, v. 79, p.1215-1225.
Harris, R.A., and Simpson, B.W.,1992, Changes in static stress on southern California faults after the 1992 Landers earthquake, Nature, Volume 360, p.251-254.
Heppe, K., Helmcke, D., and Wemmer, K.,2007, The Lancang River Zone of southwestern Yunnan, China:A questionable location for the active continental margin of Paleotethys:Journal of Asian Earth Sciences, v.30, p.706-720.
Huang, J.,2002, Lithospheric structure and its relationship to seismic and volcanic activity in southwest China:Journal of Geophysical Research, v.107, p.2255.
Jaeger, J.C., and Cook, N.G.W.,1969, Fundamentals of Rock Mechanics:London, Methuen and Co.
Joswig, M.,1990, Pattern recognition for earthquake detection:Bulletin of the Seismological Society of America, v.80, p.170-186.
Joswig, M.,1993, Single-trace detection and array-wide coincidence association of local earthquakes and explosions:Computers and Geosciences, v.19, p.207-221.
Kiimpel, H.-J.,1991, Poroelasticity:parameters reviewed:Geophys. J. Int., v.105, p.783-799.
Kagan, Y.Y.,1994, Incremental Stress and Earthquakes:Geophys. J. Int,v.117, p.345-364.
Kagan, Y.Y., and Jackson, D.D.,1998, Spatial aftershock distribution:Effect of normal stress:Journal of Geophysical Research, v.103, p.24453-24467.
Karakostas, V.G.,2003, The 2001 Skyros, Northern Aegean, Greece, earthquake sequence:off-fault aftershocks, tectonic implications, and seismicity triggering:Geophysical Research Letters, v. 30, p.1-12.
Kennet, B.L.N., and Engdahl, E.R.,1991, IASPEI 1991 seismological tables:Terra Nova, v.3, p.122.
King, G.C.P., Stein, R.S., and Lin, J.,1994, static stress changes and the triggering of earthquakes: Bulletin of the Seismological Society of America, v.84, p.935-953.
Lacassin, R., Replumaz, A., and Lelou, P.H.,1998, Hairpin river loops and slip-sense inversion on southeast Asian strike-slip faults:Geology, v.26, p.703-706.
Lawson, C.L., and Hanson, R.J.,1974, Solving Least Squares Problems:New Jersey, Prentice-Hall.
Lee, W.H.K., and Lahr, J.C.,1975, HYPO71:A computer program for determining hypocenter magnitude, and first motion pattern of local earthquakes:California, USGS.
Lei, J., Xie, F., Mishra, O.P., Lu, Y., Zhang, G., and Li, Y.,2012, The 2011 Yingjiang, China, earthquake:a volcano-related fluid-driven earthquake?:Bulletin of the Seismological Society of America, v. 102, p.417-425.
Li, C., Vanderhilst, R., Meltzer, A., and Engdahl, E.,2008a, Subduction of the Indian lithosphere beneath the Tibetan Plateau and Burma:Earth and Planetary Science Letters, v.274, p. 157-168.
Li, C., Vanderhilst, R., and Toksoz, M.,2006, Constraining P-wave velocity variations in the upper mantle beneath Southeast Asia:Physics of The Earth and Planetary Interiors, v.154, p. 180-195.
Li, Y., Wu, Q., Zhang, R., Tian, X., and Zeng, R.,2008b, The crust and upper mantle structure beneath Yunnan from joint inversion of receiver functions and Rayleigh wave dispersion data:Physics of The Earth and Planetary Interiors, v.170, p.134-146.
Liang, C.,2004, Tomographic inversion of Pn travel times in China:Journal of Geophysical Research, v. 109, p. B11304.
Lienert, B., and Havskov, J.,1995, A computer program for locating earthquakes both locally and globally:Seismological Research Letters, v.66, p.26-36.
Lomax, A., Virieux, J., Volant, P., and Berge-Thierry, C.,2000, Probabilistic Earthquake Location in 3D and Layered Models:Advances in Seismic Event Location Modern Approaches in Geophysics, v. 18, p.101-134.
Lomax, A., Zollo, A., Capuano, P., and Virieuxl, J.,2001, Precise, absolute earthquake location under Somma-Vesuvius volcano using a new three-dimensional velocity model:Geophys. J. Int., v. 146, p.313-331.
Menke, W.,1999, Using waveform similarity to constrain earthquake locations:Bulletin of the Seismological Society of America, v.89, p.1143-1146.
Mogi, K.,1979, Two kinds of seismic gaps:Pure Appl. Geophys., v.117, p.1172-1186.
Morley, C.K.,2007, Variations in Late Cenozoic-Recent strike-slip and oblique-extensional geometries, within Indochina:The influence of pre-existing fabrics:Journal of Structural Geology, v.29, p. 36-58.
Mosteller, F., and Tukey, J.W.,1977, Data analysis and regression:a second course in statistics.: Massachussets, Addison-Wesley, Reading.
Muller, G.,1977, Earth-flattening approximation for body waves derived from geometric ray theory-improvements, corrections and range of applicability:J. Geophys., v.58, p.153-174.
Murdock, J.N., and Hutt, C.R.,1983, A new event detector designed for the seismic research observatories, Volume Open File Report, USGS, p.83-7851.
Nalbant, S.S., Hubert, A., and King, G.C.P.,1998, Stress coupling between earthquakes in northwest Turkey and the north Aegean Sea:Journal of Geophysical Research, v.103, p.24469-24486.
Nielsen, C., Chamot-Rooke, N., and Rangin, C,2004, From partial to full strain partitioning along the Indo-Burmese hyper-oblique subduction:Marine Geology, v.209, p.303-327.
Paige, C.C., and Saunders, M.A.,1982, LSQR:An Algorithm for Sparse Linear Equations and Sparse Least Squares:ACM Transactions on Mathematical Software, v.8, p.43-71.
Parolai, S., Trojani, L., Monachesi, G., Frapiccini, M., Cattaneo, M., and Augliera, P.,2001, Hypocenter location accuracy and seismicity distribution in the Central Apennines (Italy):Journal of Seismology, v.5, p.243-261.
Peltzer, G., and Tapponnier, P.,1988, Formation and evolution of strike-slip faults, rifts, and basins during the India-Asia Collision:An experimental approach:Journal of Geophysical Research, v. 93, p.15085-15117.
Peppin, W.A., Honjas, W., Somerville, M.R., and Vetter, U.R.,1989, Precise master-event locations of aftershocks of the 4 October 1978 Wheeler Crest earthquake sequence near Long Valley, California:Bulletin of the Seismological Society of America, v.79, p.67-76.
Poupinet, G., Ellsworth, W.L., and Frechet, J.,1984, Monitoring velocity variations in the crust using earthquake doublets:An application to the Calaveras Fault, California:Journal of Geophysical Research, v.89, p.5719-5731.
Reasenberg, P.A., and Simpson, R.W.,1992, Response of regional seismicity to the static stress change produced by the Loma Prieta earthquake:Science, v.255, p.1687-1690.
Rice, J.R.,1992, Fault Stress States, Pore Pressure Distributions, and the Weakness of the San Andreas Fault:International Geophysics, v.51, p.475-503.
Rice, J.R., and Cleary, M.P.,1976, Some basic stress diffusion solutions for fluid-saturated elastic porous media with compressible constituents:Reviews of Geophysics, v.14, p.227-241.
Roeloffs, E., and Rudnicki, J.W.,1985, Coupled deformation-diffusion effects on water-level changes due to propagating creep events:Pure Appl. Geophys., v.122, p.560-582.
Roeloffs, E.A.,1988, Fault stability changes induced beneath a reservoir with cyclic variations in water level:Journal of Geophysical Research, v.93, p.2107-2124.
Roeloffs, E.A.,1996, Poroelastic techniques in the study of earthquake-related hydrologic phenomena: Advances in Geophysics, v.37.
Ruzek, B., and Kvasnicka, M.,2001, Differential Evolution Algorithm in the Earthquake Hypocenter Location:Pure appl. Geophys., v.158, p.667-693.
Sambridge, M.S., and Kennett, B.L.N.,1986, A novel method of hypocentre location:Geophys. J. Int., v. 87, p.679-697.
Sambridge, M.S., and Kennett, B.L.N.,2001, Seismic Event Location:Nonlinear Inversion Using a Neighbourhood Algorithm:Pure appl. Geophys., v.158, p.241-257.
Schweitzer, J.,2001, HYPOSAT - An Enhanced Routine to Locate Seismic Events:Pure appl. Geophys., v.158, p.277-289.
Shedlock, K.M., Giardini, D., GriJnthal, G., and Zhang, P.,2000, The GSHAP Global Seismic Hazard Map: Seismological Research Letters, v.71, p.679-686.
Skempton, A.W.,1954, The Pore-Pressure Coefficients A and B:Geotechnique, v.4, p.143-147.
Socquet, A., and Pubellier, M.,2005, Cenozoic deformation in western Yunnan (China-Myanmar border):Journal of Asian Earth Sciences, v.24, p.495-515.
Spence, W.,1980, Relative epicenter determination using P-wave arrival-time differences:Bulletin of the Seismological Society of America, v.70, p.171-183.
Stein, R.S., King, G.C.P., and Lin, J.,1992, Change in Failure Stress on the Southern San Andreas Fault System Caused by the 1992 Magnitude= 7.4 Landers Earthquake:Science, v.258, p.1328-1332.
Stein, S., and Wysession, M.,1991, An Introduction to Seismology, Earthquakes and Earth Structures.: Evanston, Northwesten Univercity, USA.
Tao, W., and Shen, Z.,2008, Heat flow distribution in Chinese continent and its adjacent areas: Progress in Natural Science, v.18, p.843-849.
Troise, C., De Natale, G., Pingue, F., and Petrazzuoli, S.M.,1998, Evidence for static stress interaction among earthquakes in the south-central Apennines:Geophys. J. Int., v.134, p.809-817.
Waldhauser, F.,2001, HYPODD-A program to compute double-difference hypocenter locations: California, U. S. Geologic Survey.
Waldhauser, F., and Ellsworth, W.L.,2000, A double-difference earthquake location algorithm:method and application to the northern Hayward fault, California:Bulletin of the Seismological Society of America, v.90, p.1353-1368.
Wang, and C.,2004, Crustal structure in Tengchong Volcano-Geothermal Area, western Yunnan, China: Tectonophysics, v.380, p.69-87.
Wang, C.-Y.,2003, Three-dimensional velocity structure of crust and upper mantle in southwestern China and its tectonic implications: Journal of Geophysical Research, v.108, p.2442.
Wang, E., and Burchfiel, B.C.,1997, Interpretation of Cenozoic Tectonics in the Right-Lateral Accommodation Zone Between the Ailao Shan Shear Zone and the Eastern Himalayan Syntaxis:International Geology Review, v.39, p.191-219.
Wang, Y, Fan, W., Zhang, Y., Peng, T., Chen, X., and Xu, Y.,2006, Kinematics and 40Ar/39Ar geochronology of the Gaoligong and Chongshan shear systems, western Yunnan, China: Implications for early Oligocene tectonic extrusion of SE Asia:Tectonophysics, v.418, p. 235-254.
Wells, D.L., and Coppersmith, K.J.,1994, New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement:Bulletin of the Seismological Society of America, v.84, p.974-1002.
Wiechert, E., and Zoeppritz, K.,1907, Ueber erdbebenwellen:Nachrichten von der Gesellschaft der Wissenschaften zu Gottingen, Mathematisch-Physikalische Klasse, p.413-529.
Xiong, X., Shan, B., Zheng, Y, and Wang, R.,2010, Stress transfer and its implication for earthquake hazard on the Kunlun Fault, Tibet:Tectonophysics, v.482, p.216-225.
Xu, L., Rondenay, S., and van der Hilst, R.D.,2007, Structure of the crust beneath the southeastern Tibetan Plateau from teleseismic receiver functions:Physics of The Earth and Planetary Interiors, v.165, p.176-193.
Yang, Z., Chen, Y., and Zhang, H.,2002, Relocation and seismogenic structure of the 1998 Zhangbei-Shangyi earthquake sequence:Acta Seismologica Sinica, v.15, p.383-394.
Zhang, X., and Wang, Y.,2009, Crustal and upper mantle velocity structure in Yunnan, Southwest China: Tectonophysics, v.471, p.171-185.
Zhao, D.,2007, Seismic images under 60 hotspots:Search for mantle plumes:Gondwana Research, v. 12, p.335-355.
Zhao, D.,2009, Multiscale seismic tomography and mantle dynamics:Gondwana Research, v.15, p. 297-323.
Zhou, H., Liu, H.-L., and Kanamori, H.,1983, Source processes of large earthquakes along the Xianshuihe fault in southwestern China:Bulletin of the Seismological Society of America, v.73, p.537-551.
万永革,吴忠良,周公威,and黄静,2000,几次复杂地震中不同破裂事件之间的“应力触发”问题：地震学报,v.22,p.568-576.
毛玉平,韩新民,and谷一山,2003,云南地区强震(M≥6)研究：昆明,云南科技出版社.
王刚,万景林,and王二七,2006,高黎贡山脉南部的晚新生代构造—重力垮塌及其成因：地质学报,v.80,p.1262-1273.
王晋南,王洋龙,安晓文,杨向东,and常祖峰,2006,1976年龙陵地震区断裂活动性研究：地震研究,v.29,p.366-372.
王阎昭,王恩宁,沈正康,王敏,甘卫军,乔学军,孟国杰,李铁明,陶玮,杨永林,程佳,and李鹏,2008,基于GP5资料约束反演川滇地区主要断裂现今活动速率：中国科学(D辑),v.38,p.582-597.
付虹,黄浩,李丽,and赵小艳,2011,2011年3月10日云南盈江5.8级地震序列研究：地震研究v.34,p.414-419.
田玥,and陈晓非,2002,地震定位研究综述：地球物理学进展,v.17,p.147-155.
安晓文,常祖峰,and石静芳,2009,大盈江断裂西南段晚第四纪活动研究：地震研究,v.32,p.193-197.
朱成男,1979,龙陵地震地质背景：地震研究,p.53-64.
李四光,1973,地质力学概论：北京,科学出版社.
李四光,1974,旋扭构造：北京,科学出版社.
李四光,1979,地质力学方法：北京,科学出版社.
杜义,张效亮,黄学猛,杜宇本,and谢富仁,2012,龙陵-瑞丽断裂北段晚第四纪活动性特征及强震复发间隔：震灾防御技术,v.7,p.215-226.
周立功,1983,微震台网在地质工作中的应用：中国地质,p.21-26.
房立华,吴建平,张天中,黄静,王长在,and杨婷,2011,2011年云南盈江Ms5.8地震及其余震序列重定位：地震学报,v.33,p.262-267.
姚鑫,张加桂,张永双,杨波,and余凯,2011,2011年3月10日盈江5.8级地震诱发砂土液化灾害特征研究：工程地质学报,v.2,p.152-161.
胡鸿翔,林中洋,边银菊,王椿镛,and朱良保,1996,滇西地区壳幔慢过渡带性质的研究：地震学报,v.18,p.444-450.
胡鸿翔,陆涵行,and 王椿镛,1993,滇西地区地壳浅部基底速度细结构的研究：中国地震,v.9,p.356-364.
胡鸿翔,陆涵行,王椿铺,何正勤,and朱良保,1986,滇西地区地壳结构的爆破地震研究：地球物理学报,v.29,p.133-144.
徐纪人,赵志新,and石川有三,2008,中国大陆地壳应力场与构造运动区域特征研究：地球物理学报,v.51,p.770-781.
常祖峰,安晓文,and张艳凤,2012,畹町断裂晚第四纪活动与水系构造变形：地震地质,v.34,p.228-239.
常祖峰,陈刚,and余建强,2011,大盈江断裂晚更新世以来活动的地质证据：地震地质,v.33,p.877-888.
傅竹武,王苏,刘建华,and胥颐,2007a,利用接收函数方法研究瑞丽—龙陵断裂两侧S波速度结构：地震研究,v.30,p.223-228.
傅竹武,刘建华,胥颐,文丽敏,续外芬,and马红虎,2007b,利用接收函数方法研究大盈江断裂两侧S波速度结构：云南大学学报,v.29,p.607-612.
傅淑芳,and刘宝诚,1991,地震学教程：北京,地震出版社,447-480 p.
樊春,and王二七,2004,滇西高黎贡山南段左行剪切构造形迹的发现及其大地构造意义：自然科学进展,v.14,p.1189-1193.
虢顺民,向宏发,周瑞琦,徐锡伟,董兴权,and张晚霞,1999,滇西南龙陵—澜沧断裂带——大陆地壳上一条新生的破裂带：科学通报,v.44,p.2118-2121.
虢顺民,向宏发,徐锡伟,张晚霞,周瑞琦,and 董兴权,2000,滇西南龙陵—澜沧第四纪新生断裂带特征和形成机制研究：地震地质,v.22,p.277-284.
冯梅,安美健,王小凤,and马寅生,2007,青海狮子沟油田天然微地震活动及其地质意义：地质力学学报,v.13,p.173-178.
吴中海,李贵书,毛晓长,尹福光,翟刚毅,and张虎,2013,泛业铁路云南大理至瑞丽沿线基础地质与主要工程地质问题：北京,地质出版社.
吴中海,赵希涛,范桃园,叶培盛,仝亚博,and杨振宇,2012,泛亚铁路滇西大理至瑞丽沿线主要活动断裂与地震地质特征：地质通报,v.31,p.191-217.
孙泽轩,2000,盈江盆地盖层氧化带发育特征及其与铀矿化的关系：铀矿地质,v.16,p.79-84.
张小涛,吕坚,and 马广庆,2008,双差地震定位法在邯郸—邢台地区地震精确定位中的初步应用：地震研究,v.31,p.37-41.
张中杰,白志明,王椿镛,吕庆田,滕吉文,李继亮,孙善学,and王新征,2005,冈瓦纳型和扬子型地块地壳结构：以滇西孟连—马龙宽角反射剖面为例：中国科学D辑,v.34,p.387-392.
张四昌,刁桂苓,王绍晋,and龙晓帆,1994,1976年龙陵震群序列的破裂特征：中国地震,v.10,p.152-159.
张四昌,and徐杰,1978,1976年龙陵地震地震地质特征的探讨：地震研究,p.44-54.
张永北,1999,龙陵—瑞丽走滑体系中段自相似结构与热液成矿定位：地质学报,v.73,p.334-341.
杨中书,and曾文敬,2007,利用双差法对2005年江西九江—瑞昌5.7级地震序列重新定位：地震地磁观测与研究,v.28,p.25-31.
杨晶琼,杨周胜,and刘丽芳,2010a,2008年盈江5.9级地震序列震源参数研究：地震研究,v.33,p.308-312.
杨晶琼,杨周胜,刘丽芳,苏有锦,and张森,2010b,2008年盈江5.9级地震序列震源参数研究：地震研究,v.33,p.308-312.
杨智娴,陈运泰,郑月军,and于湘伟,2003,双差地震定位法在我国中西部地区地震精确定位中的应用：中国科学(D辑),v.33,p.129-134.
许忠淮,2001,东亚地区现今构造应力图的编制：地震学报,v.23,p.492-501.
许忠淮,汪素云,黄雨蕊,and高阿甲,1989,山大量的地震资料推断的我国大陆构造应力场：地球物理学报,v.32,p.636-647.
谢韬,林仕良,李富,丛峰,李再会,and邹光富,2011,龙陵—瑞丽断裂潞西段的发育特征及意义大地构造与成矿学,v.35,p.216-220.
郑钰,and杨建思,2008,双差算法的剖析及参数对定位的影响：地震地磁观测与研究,v.29,p.85-93.
钱晓东,苏有锦,付虹,and李琼,2011,2011年云南盈江5.8级地震及震前短临跟踪预测：地震研究,34,p.403-413.
阚荣举,王绍晋,and刘祖荫,1979,龙陵地震序列的震源机制特征,p.10-21.
阚荣举,and彭万里,1980,西南地区应力场变动与强震活动秩序及实验研究：地震研究,v.3,p.181-192.
陈立德,and赵维城,1979,1976年龙陵地震：北京,地震出版社.
陈顒,and黄庭芳,2001,岩石物理学：北京,北京大学出版社.
马瑾,1987,构造物理学概论：北京,地震出版社.
黄学猛,杜义,舒赛兵,and谢富仁,2010,龙陵—瑞丽断裂(南支)北段晚第四纪活动性特征：地震地质,v.32,p.222-232.
黄崐,万建平,and黄莺,1987,1976年龙陵地区地震前后垂直形变的演变过程：地震研究,v.10,p.671-680.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |