龙门山断裂带东北段现今地应力环境研究
|
摘要
2008年5月12日汶川MS8.0级地震后,为了解发震断裂附近地应力分布特征,于2009年10月-12月期间,在龙门山断裂带东北段江油、北川地区3个200m钻孔中开展水压致裂地应力测量工作;本文首先依据研究区域内3个200m钻孔的水压致裂地应力测量结果,分析了汶川8.0级地震发生1年后,龙门山断裂带东北段附近现今地应力状态分布特征;其次,基于龙门山断裂带基础地质、地球物理等研究资料,采用线弹性有限元模拟方法,运用ANSYS有限元模拟软件,模拟得到了地震后研究区内现今地应力状态;再次,综合研究区内地应力测量结果和应力场的三维有限元数值模拟结果,揭示了断裂带附近江油～北川剖面现今应力场的变化规律;文章最后探讨了龙门山断裂带东北段江油和北川地区的地震危险性.
After Wenchuan MS 8.0 earthquake occurred on the May 12th 2008,in Sichuan province,China,in an attempt to understand the distribution of the in situ stress near the fault,we made a series of in situ stress measurements in three 200 m-deep boreholes drilled in Beichuan and Jiangyou areas near the northeastern segment of Longmenshan fault belt,in 2009,using the hydraulic fracturing technique.Firstly,according to the in-situ stress results with the method of hydraulic fracturing measurement in three 200 m-deep boreholes in the region,the distribution characterizes of current in-situ stress state near the northern segment of Longmenshan fault was analyzed over one year after Wenchuan MS 8.0 earthquake.Secondly,on basis of foundational geological data of Longmenshan fault,we calculate the present stress state by the method of linear elastic finite element numerical simulation with ANSYS.Thirdly,combined the in situ stress measurements with the simulation results,the variation of the stress state along the profile between Jiangyou and Beichuan is revealed.Finally,seismic risk in Jiangyou and Beichuan areas along the northern segment of Longmenshan fault is discussed.
After Wenchuan MS 8.0 earthquake occurred on the May 12th 2008,in Sichuan province,China,in an attempt to understand the distribution of the in situ stress near the fault,we made a series of in situ stress measurements in three 200 m-deep boreholes drilled in Beichuan and Jiangyou areas near the northeastern segment of Longmenshan fault belt,in 2009,using the hydraulic fracturing technique.Firstly,according to the in-situ stress results with the method of hydraulic fracturing measurement in three 200 m-deep boreholes in the region,the distribution characterizes of current in-situ stress state near the northern segment of Longmenshan fault was analyzed over one year after Wenchuan MS 8.0 earthquake.Secondly,on basis of foundational geological data of Longmenshan fault,we calculate the present stress state by the method of linear elastic finite element numerical simulation with ANSYS.Thirdly,combined the in situ stress measurements with the simulation results,the variation of the stress state along the profile between Jiangyou and Beichuan is revealed.Finally,seismic risk in Jiangyou and Beichuan areas along the northern segment of Longmenshan fault is discussed.
引文
[1]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.
[2]Liao C T,Zhang C S,Wu M L,et al.Stress change near theKunlun Fault before and after the Ms8.1Kunlun Earthquake[J].Geophys.Res.Lett.,2003,30(20):2027-2030.
[3]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):1395-1401.Guo Q L,Wang C H,Ma H S,et al.In-situ hydro-fracturestress measurement before and after the Wenchuan MS8.0earthquake of China[J].Chinese J.Geophys.(in Chinese),2009,52(5):1395-1401.
[4]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.
[5]中国地震局监测预报司.汶川8.0级地震科学研究报告[M].北京:地震出版社,2009:1-2.Department of Earthquake Monitoring and Prediction,ChinaEarthquake Administration.A scientific research report ofMs8.0 Wenchuan earthquake[M].Beijing:SeismologicalPress(in Chinese),2009:1-2.
[6]张培震,邓起东,张国民,等.中国大陆的强震活动与活动地块[J].中国科学D辑:地球科学,2003,33(增刊):12-20.Zhang P Z,Deng Q D,Zhang G M,et al.Activity of strongearthquake and active block in Mainland China[J].Science inChina Series D:Earth Science(in Chinese),2003,33(supplement):12-20.
[7]易桂喜,闻学泽,王思维,等.由地震活动参数分析龙门山-岷山断裂带的现今活动习性与强震危险性[J].中国地震,2006,22(2):117-125.Yi G X,Wen X Z,Wang S W,et al.Study on fault slidingbehaviors and strong-earthquake risk of the Longmenshan-Minshan fault zones from current seismicity parameters[J].Earthquake Research in China(in Chinese),2006,22(2):117-125.
[8]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):389-402.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.
[9]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.
[10]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.
[11]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:地球科学,2008,38(9):1041-1055.Zhang P Z.Recent tectonic deformation,distribution ofstrain and the deep dynamical process in the western Sichuanregion at the eastern margin of the Tibetan Plateau[J].Science in China Series D:Earth Science(in Chinese),2008,38(9):1041-1055.
[12]国家地震局震害防御司.中国历史强震目录[M].北京:地震出版社,1995:1-514.Department of Earthquake Monitoring and Prediction,ChinaEarthquake Administration.Catalogue of Chinese historicalstrong earthquakes[M].Beijing:Seismological Press(inChinese),1995:1-514.
[13]唐文清,刘宇平,陈智梁,等.龙门山断裂构造带GPS研究[J].大地测量与地球动力学,2004,24(3):57-60.Tang W Q,Liu Y P,Chen Z N,et al.GPS study onLongmenshan fault zone[J].Crustal Deformation andEarthquake(in Chinese),2004,24(3):57-60.
[14]李勇,周荣军,董顺利,等.汶川地震的地表破裂与逆冲-走滑作用[J].成都理工大学学报(自然科学版),2008,35(4):404-413.Li Y,Zhou R J,Dong S L,et al.Surface rupture,thrustingand strike-slipping in the Wenchuan earthquake of Sichuan,China.[J].Journal of Chengdu University of Technology(Science and Technology Edition)(in Chinese),2008,35(4):404-413.
[15]唐荣昌,黄祖智,周荣军,等.四川活断层分段与强震危险性概率预测[J].中国地震,1995,11(3):272-282.Tang R C,Huang Z Z,Zhou R J,et al.Segmentation ofactive fault and risk probability prediction of strongearthquakes in Sichuan province[J].Earthquake ResearchChina(in Chinese),1995,11(3):272-282.
[16]唐荣昌,韩渭宾.四川活动断裂与地震[M].北京:地震出版社,1993:123-132.Tang R C,Han W B.Active fault and earthquake in Sichuanprovince[M].Beijing:Seismological Press(in Chinese),1993:123-132.
[17]李勇,周荣军,DensmoreA L,等.青藏高原东缘龙门山晚新生代走滑挤压作用的沉积响应[J].沉积学报,2006,24(2):153-164.Li Y,Zhou R J,Densmore A L,et al.Sedimentaryresponses to late Cenozoic thrusting and strike-slipping ofLongmen Shan along eastern margin of Tibetan Plateau[J].Acta Sedimentologica Sinica(in Chinese),2006,24(2):153-164.
[18]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.
[19]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&MiningSciences,2003,40(7-8):1011-1020.
[20]白世伟,李光煜.二滩水电站坝区岩体应力场研究[J].岩石力学与工程学报,1982,1(1):46-55.Bai S W,Li G Y.Research on stress field around dam area ofErtan Hydropower station[J].Chinese Journal of RockMechanics and Engineering(in Chinese),1982,1(1):46-55.
[21]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].CrustalDeformation and Earthquake(in Chinese),2004,24(2):115-119.
[22]刘光勋,李方全,李桂荣.我国滇西北地震活动区的活动构造与应力状态[J].地震地质,1986,8(1):1-14.Liu G X,Li F Q,Li G R.Active tectonics and state of stressin seismic region of north-west Yunnan province,China[J].Seismology and Geology(in Chinese),1986,8(1):1-14.
[23]Tanaka Y,Nakajima T,Saito T.The Crustal stress field inthe Japanese Islang-ageneral view of the results of in situstress measurements[J].Journal of Geod.Soc.Jpn,1981,26:322-326.
[24]Zoback M D,Roller J C.Magnitude of shear stress on theSan Andreas fault:Implications of a stress measurementprofile at shallow depth[J].Science,1979,206(4417):445-447.
[25]Zoback M D,Tsukara H,Hickman S.Stress measurementsat depth in the vicinity of the San Andreas Fault:Implicationsfor the magnitude of shear stress at depth[J].Journal ofGeophysical Research,1980,85(B11):6157-6173.
[26]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):74-86.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):74-86.
[27]谢富仁,陈群策,崔效锋,等.中国大陆地壳应力环境研究[M].北京:地质出版社,2003:1-39.Xie F R,Chen Q C,Cui X F,et al.Crustal stress in China[M].Beijing:Geological Publishing House(in Chinese),2003:1-39.
[28]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,2012,52(12):4027-4217.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),2012,52(12):4027-4217.
[29]胡幸平,俞春泉,陶开,等.利用P波初动资料求解汶川地震及其强余震震源机制解[J].地球物理学报,2008,51(6):1711-1718.Hu X P,Yu C Q,Tao K,et al.Focal mechanism solutionsof Wenchuan earthquake and its strong aftershocks obtainedfrom initial P wave polarity analysis[J].Chinese J.Geophys.(in Chinese),2008,51(6):1711-1718.
[30]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.
[31]李方全,王连捷.华北地区地应力测量[J].地球物理学报,1979,22(1):1-8.Li F Q,Wang L J.Stress measurements in north China[J].Chinese J.Geophys.(in Chinese),1979,22(1):1-8.
[32]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 measurement at the northeastern section of theLongmenshan fault zone after the 5.12 Wenchuanearthquake[J].Chinese J.Geophys.(in Chinese),2012,55(12):3923-3932.
[33]谭成轩,孙炜锋,孙叶,等.地应力测量及其地下工程应用的思考[J].地质学报,2006,80(10):1627-1632.Tan C X,Sun W F,Sun Y,et al.A consideration on in-situcrustal stress measuring and its underground engineeringapplication[J].Acta Geologica Sinica(in Chinese),2006,80(10):1627-1632.
[34]Byerlee J O.Friction of rocks[J].Pure and Applied Geophysics,1978,116(4-5):615-626.
[35]李宏,谢富仁,王海忠,等.乌鲁木齐市断层附近地应力特征与断层活动性[J].地球物理学报,2012,55(11):3690-3698.Li H,Xie F R,Wang H Z,et al.Characteristics of in-situstress measurements near the fault and fault activity inUrumqi City[J].Chinese J.Geophys.(in Chinese),2012,55(11):3690-3698.
[36]王艳华,崔效锋,胡辛平,等.基于原地应力测量数据的中国大陆地壳上部应力状态研究[J].地球物理学报,2012,55(9):3016-3027.Wang Y H,Cui X F,Hu X P,et al.Study on the stressstate in upper crust of China mainland based on in-situ stressmeasurements[J].Chinese J.Geophys.(in Chinese),2012,55(9):3016-3027.
[37]王成虎,丁立丰,李方全,等.川西北跨度23a的原地应力实测数据特征及其地壳动力学意义分析[J].岩石力学与工程学报,2012,31(11):2171-2181.Wang C H,Ding L F,Li F Q,et al.Characteristics of in-situ stress measurement in northwest Sichuan basin withtimespan of 23years and its crustal dynamics significance[J].Chinese Journal of Rock Mechanics and Engineering(inChinese),2012,31(11):2171-2181.
[38]田中丰,藤森邦夫,大塚成昭.地壳应力歪の测定观测による大地震发生の预测[J].地震,1998,50(2):201-208.
[2]Liao C T,Zhang C S,Wu M L,et al.Stress change near theKunlun Fault before and after the Ms8.1Kunlun Earthquake[J].Geophys.Res.Lett.,2003,30(20):2027-2030.
[3]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):1395-1401.Guo Q L,Wang C H,Ma H S,et al.In-situ hydro-fracturestress measurement before and after the Wenchuan MS8.0earthquake of China[J].Chinese J.Geophys.(in Chinese),2009,52(5):1395-1401.
[4]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.
[5]中国地震局监测预报司.汶川8.0级地震科学研究报告[M].北京:地震出版社,2009:1-2.Department of Earthquake Monitoring and Prediction,ChinaEarthquake Administration.A scientific research report ofMs8.0 Wenchuan earthquake[M].Beijing:SeismologicalPress(in Chinese),2009:1-2.
[6]张培震,邓起东,张国民,等.中国大陆的强震活动与活动地块[J].中国科学D辑:地球科学,2003,33(增刊):12-20.Zhang P Z,Deng Q D,Zhang G M,et al.Activity of strongearthquake and active block in Mainland China[J].Science inChina Series D:Earth Science(in Chinese),2003,33(supplement):12-20.
[7]易桂喜,闻学泽,王思维,等.由地震活动参数分析龙门山-岷山断裂带的现今活动习性与强震危险性[J].中国地震,2006,22(2):117-125.Yi G X,Wen X Z,Wang S W,et al.Study on fault slidingbehaviors and strong-earthquake risk of the Longmenshan-Minshan fault zones from current seismicity parameters[J].Earthquake Research in China(in Chinese),2006,22(2):117-125.
[8]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):389-402.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.
[9]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.
[10]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.
[11]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:地球科学,2008,38(9):1041-1055.Zhang P Z.Recent tectonic deformation,distribution ofstrain and the deep dynamical process in the western Sichuanregion at the eastern margin of the Tibetan Plateau[J].Science in China Series D:Earth Science(in Chinese),2008,38(9):1041-1055.
[12]国家地震局震害防御司.中国历史强震目录[M].北京:地震出版社,1995:1-514.Department of Earthquake Monitoring and Prediction,ChinaEarthquake Administration.Catalogue of Chinese historicalstrong earthquakes[M].Beijing:Seismological Press(inChinese),1995:1-514.
[13]唐文清,刘宇平,陈智梁,等.龙门山断裂构造带GPS研究[J].大地测量与地球动力学,2004,24(3):57-60.Tang W Q,Liu Y P,Chen Z N,et al.GPS study onLongmenshan fault zone[J].Crustal Deformation andEarthquake(in Chinese),2004,24(3):57-60.
[14]李勇,周荣军,董顺利,等.汶川地震的地表破裂与逆冲-走滑作用[J].成都理工大学学报(自然科学版),2008,35(4):404-413.Li Y,Zhou R J,Dong S L,et al.Surface rupture,thrustingand strike-slipping in the Wenchuan earthquake of Sichuan,China.[J].Journal of Chengdu University of Technology(Science and Technology Edition)(in Chinese),2008,35(4):404-413.
[15]唐荣昌,黄祖智,周荣军,等.四川活断层分段与强震危险性概率预测[J].中国地震,1995,11(3):272-282.Tang R C,Huang Z Z,Zhou R J,et al.Segmentation ofactive fault and risk probability prediction of strongearthquakes in Sichuan province[J].Earthquake ResearchChina(in Chinese),1995,11(3):272-282.
[16]唐荣昌,韩渭宾.四川活动断裂与地震[M].北京:地震出版社,1993:123-132.Tang R C,Han W B.Active fault and earthquake in Sichuanprovince[M].Beijing:Seismological Press(in Chinese),1993:123-132.
[17]李勇,周荣军,DensmoreA L,等.青藏高原东缘龙门山晚新生代走滑挤压作用的沉积响应[J].沉积学报,2006,24(2):153-164.Li Y,Zhou R J,Densmore A L,et al.Sedimentaryresponses to late Cenozoic thrusting and strike-slipping ofLongmen Shan along eastern margin of Tibetan Plateau[J].Acta Sedimentologica Sinica(in Chinese),2006,24(2):153-164.
[18]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.
[19]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&MiningSciences,2003,40(7-8):1011-1020.
[20]白世伟,李光煜.二滩水电站坝区岩体应力场研究[J].岩石力学与工程学报,1982,1(1):46-55.Bai S W,Li G Y.Research on stress field around dam area ofErtan Hydropower station[J].Chinese Journal of RockMechanics and Engineering(in Chinese),1982,1(1):46-55.
[21]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].CrustalDeformation and Earthquake(in Chinese),2004,24(2):115-119.
[22]刘光勋,李方全,李桂荣.我国滇西北地震活动区的活动构造与应力状态[J].地震地质,1986,8(1):1-14.Liu G X,Li F Q,Li G R.Active tectonics and state of stressin seismic region of north-west Yunnan province,China[J].Seismology and Geology(in Chinese),1986,8(1):1-14.
[23]Tanaka Y,Nakajima T,Saito T.The Crustal stress field inthe Japanese Islang-ageneral view of the results of in situstress measurements[J].Journal of Geod.Soc.Jpn,1981,26:322-326.
[24]Zoback M D,Roller J C.Magnitude of shear stress on theSan Andreas fault:Implications of a stress measurementprofile at shallow depth[J].Science,1979,206(4417):445-447.
[25]Zoback M D,Tsukara H,Hickman S.Stress measurementsat depth in the vicinity of the San Andreas Fault:Implicationsfor the magnitude of shear stress at depth[J].Journal ofGeophysical Research,1980,85(B11):6157-6173.
[26]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):74-86.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):74-86.
[27]谢富仁,陈群策,崔效锋,等.中国大陆地壳应力环境研究[M].北京:地质出版社,2003:1-39.Xie F R,Chen Q C,Cui X F,et al.Crustal stress in China[M].Beijing:Geological Publishing House(in Chinese),2003:1-39.
[28]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,2012,52(12):4027-4217.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),2012,52(12):4027-4217.
[29]胡幸平,俞春泉,陶开,等.利用P波初动资料求解汶川地震及其强余震震源机制解[J].地球物理学报,2008,51(6):1711-1718.Hu X P,Yu C Q,Tao K,et al.Focal mechanism solutionsof Wenchuan earthquake and its strong aftershocks obtainedfrom initial P wave polarity analysis[J].Chinese J.Geophys.(in Chinese),2008,51(6):1711-1718.
[30]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.
[31]李方全,王连捷.华北地区地应力测量[J].地球物理学报,1979,22(1):1-8.Li F Q,Wang L J.Stress measurements in north China[J].Chinese J.Geophys.(in Chinese),1979,22(1):1-8.
[32]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 measurement at the northeastern section of theLongmenshan fault zone after the 5.12 Wenchuanearthquake[J].Chinese J.Geophys.(in Chinese),2012,55(12):3923-3932.
[33]谭成轩,孙炜锋,孙叶,等.地应力测量及其地下工程应用的思考[J].地质学报,2006,80(10):1627-1632.Tan C X,Sun W F,Sun Y,et al.A consideration on in-situcrustal stress measuring and its underground engineeringapplication[J].Acta Geologica Sinica(in Chinese),2006,80(10):1627-1632.
[34]Byerlee J O.Friction of rocks[J].Pure and Applied Geophysics,1978,116(4-5):615-626.
[35]李宏,谢富仁,王海忠,等.乌鲁木齐市断层附近地应力特征与断层活动性[J].地球物理学报,2012,55(11):3690-3698.Li H,Xie F R,Wang H Z,et al.Characteristics of in-situstress measurements near the fault and fault activity inUrumqi City[J].Chinese J.Geophys.(in Chinese),2012,55(11):3690-3698.
[36]王艳华,崔效锋,胡辛平,等.基于原地应力测量数据的中国大陆地壳上部应力状态研究[J].地球物理学报,2012,55(9):3016-3027.Wang Y H,Cui X F,Hu X P,et al.Study on the stressstate in upper crust of China mainland based on in-situ stressmeasurements[J].Chinese J.Geophys.(in Chinese),2012,55(9):3016-3027.
[37]王成虎,丁立丰,李方全,等.川西北跨度23a的原地应力实测数据特征及其地壳动力学意义分析[J].岩石力学与工程学报,2012,31(11):2171-2181.Wang C H,Ding L F,Li F Q,et al.Characteristics of in-situ stress measurement in northwest Sichuan basin withtimespan of 23years and its crustal dynamics significance[J].Chinese Journal of Rock Mechanics and Engineering(inChinese),2012,31(11):2171-2181.
[38]田中丰,藤森邦夫,大塚成昭.地壳应力歪の测定观测による大地震发生の预测[J].地震,1998,50(2):201-208.
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心