紫坪铺水库区域地壳Q_s成像及其与渗透关系研究
|
摘要
利用衰减结构层析成像方法尝试对紫坪铺水库区域地壳Qs进行成像,获得该区浅层地壳静态及蓄水前、后的Qs变化特征,结合实验研究成果、岩体岩性、断裂构造、水文地质条件探讨库水的渗透作用及其对地壳介质的影响,对研究区内地震活动类型及发震成因的介质物性变化进行了讨论.研究结果表明:紫坪铺水库区域地壳Qs横向不均匀变化显著,库区周边近似存在低Qs值环形区域,主要包括水库东北、东南、西南、西北及库区中段五个区域.其中,水库东北、库区中段、西南低Qs区域与库水渗透关系密切,初步认为库水可能沿着通济场断裂中段和两端的岩石破碎带及节理、裂隙发育地区向地下渗透,使岩石孔隙中充满流体,内摩擦增大,地震波大大衰减,从而导致Qs值大幅下降.同时,在西南区诱发了水库小震群,在东北区和东南区诱发了部分水库小震群.另外,紫坪铺水库区域东北、东南、西南三个小震群基本位于高Qs值(低衰减)和低Qs值(高衰减)过渡区域,可能由于低Qs区地震波衰减大,不易积累能量,而高、低Qs值的过渡区域,介质介于"软"、"硬"之间,有可能积累应变能,孕育地震.当高、低Qs过渡区域岩石裂纹饱含水或部分含水后,水对裂纹边界起潮湿和润滑作用,降低了发震断层的抗剪强度,使滑动容易产生,从而诱发地震.
The crustal Qs values are imaged in Zipingpu Reservoir Area to obtain shallow crustal characteristics of Qs variation before and after the impoundment of water through two-dimensional seismic attenuation tomography.The infiltration of reservoir water and its impact on the crust are investigated with experimental findings,rocks lithology,faults,hydrological and geological conditions.Simultaneously,we discussed the type of seismic activity and physical variety of medium about the cause of earthquake occurrence in the area.The results show that there is a significant lateral heterogeneity in Qs distribution in Zipingpu Reservoir Area.Approximately,there are low Qs value annular regions surrounding the reservoir,namely,the Qs values are low on the northeast,southeast,southwest,northwest sides and in the middle part of the reservoir.Particularly,the Qs values variation are most closely related to fluid infiltration in the middle part and on the northeast,southwest sides of the reservoir.We consider that the reservoir water infiltrates through from the middle part and two sides of the rock fracture zones,joints and fractured regions of the Tongjichang faults,filling with fluid in the rock pores,increasing the internal friction,causing significant attenuation of seismic waves,resulting in a substantial decline in the value of Qs,inducing small earthquake swarms on the southwest and partly on northeast and southeast sides.The small earthquake swarms in northeast,southeast and southwest regions are basically converged to transitional edge regions of high and low Qs values.This is perhaps a result of accumulation of strain energy in weak and soft zones.After full or partial filling of water in rock cracks,there are wet and lubricating effect on the crack boundary in the high and low Qs transition region,reducing the shear strength of seismogenic faults,inducing earthquakes.
The crustal Qs values are imaged in Zipingpu Reservoir Area to obtain shallow crustal characteristics of Qs variation before and after the impoundment of water through two-dimensional seismic attenuation tomography.The infiltration of reservoir water and its impact on the crust are investigated with experimental findings,rocks lithology,faults,hydrological and geological conditions.Simultaneously,we discussed the type of seismic activity and physical variety of medium about the cause of earthquake occurrence in the area.The results show that there is a significant lateral heterogeneity in Qs distribution in Zipingpu Reservoir Area.Approximately,there are low Qs value annular regions surrounding the reservoir,namely,the Qs values are low on the northeast,southeast,southwest,northwest sides and in the middle part of the reservoir.Particularly,the Qs values variation are most closely related to fluid infiltration in the middle part and on the northeast,southwest sides of the reservoir.We consider that the reservoir water infiltrates through from the middle part and two sides of the rock fracture zones,joints and fractured regions of the Tongjichang faults,filling with fluid in the rock pores,increasing the internal friction,causing significant attenuation of seismic waves,resulting in a substantial decline in the value of Qs,inducing small earthquake swarms on the southwest and partly on northeast and southeast sides.The small earthquake swarms in northeast,southeast and southwest regions are basically converged to transitional edge regions of high and low Qs values.This is perhaps a result of accumulation of strain energy in weak and soft zones.After full or partial filling of water in rock cracks,there are wet and lubricating effect on the crack boundary in the high and low Qs transition region,reducing the shear strength of seismogenic faults,inducing earthquakes.
引文
[1]陈颙,黄庭芳,刘恩儒.岩石物理学.合肥:中国科学技术大学出版社,2009.Chen Y,Huang T F,Liu E R.Rock Physics(in Chinese).Hefei:China Science and Technology University Press,2009.
[2]王大兴,辛可锋,李幼铭等.地层条件下砂岩含水饱和度对波速及衰减影响的实验研究.地球物理学报,2006,49(3):908-914.Wang D X,Xin K F,Li Y M,et al.An experimental studyof influence of water saturation on velocity and attenuation insandstone under stratum conditions.Chinese J.Geophys.(inChinese),2006,49(3):908-914.
[3]刘建华,胥颐,郝天珧.地震波衰减的物理机制研究.地球物理学进展,2004,19(1):1-7.Liu J H,Xu Y,Hao T Y.Study on physical mechanism ofthe seismic wave attenuation.Progress in Geophysics(inChinese),2004,19(1):1-7.
[4]Sato Y.Attenuation,dispersion,and the wave guide of the Gwave.Bull.Seism.Soc.Am.,1958,48(3):231-251.
[5]Anderson D L,Archambeau C B.The anelasticity of theearth.J.Geophys.Res.,1964,69(10):2071-2084.
[6]Haydar J,AI-Shukri H K,Mitchell B J.Three-dimensionalattenuation structure in and around the new Madrid seismiczone.Bull.Seism.Soc.Ain.,l990,80(3):615-632.
[7]Hansen S,Thurber C,Mandernach M,et al.Seismicvelocity and attenuation structure of the east rift zone andsouth Flank of Kilauea volcano,Hawaii.Bulletin of theSeismological Society of America,2004,94(4):1430-1440.
[8]丛连理,胡家富,傅竹武等.中国大陆及邻近地区Lg尾波的Q值分布.中国科学(D辑),2002,32(8):617-624.Cong L L,Hu J F,Fu Z W,et al.Distribution Lg coda Q-value in China and its neighboring regions.Science in China(Series D)(in Chinese),2002,32(8):617-624.
[9]洪学海,朱介寿,曹家敏等.中国大陆地壳上地幔S波品质因子三维层析成像.地球物理学报,2003,46(5):642-651.Hong X H,Zhu J S,Cao J M,et al.Tomography of the 3-DS-wave quality factor of the crust and upper mantle in China.Chinese J.Geophys.(in Chinese),2003,46(5):642-651.
[10]Pei S P,Zhan J M,Rowe C A,et al.MLamplitudetomography in North China.Bull.Seismo.Soc.Am.,2006,96(4A):1560-1566.
[11]马宏生,汪素云,裴顺平等.川滇及周边地区地壳横波衰减的成像研究.地球物理学报,2007,50(2):465-471.Ma H S,Wang S Y,Pei S P,et al.Q0tomography of S waveattenuation in Sichuan-yunnan and adjacent regions.ChineseJ.Geophys.(in Chinese),2007,50(2):465-471.
[12]汪素云,裴顺平,许忠淮等.利用ML振幅研究地壳横波Q值I:不同构造区的衰减特征.地球物理学报,2007,50(6):1740-1747.Wang S Y,Pei S P,Xu Z H,et al.Crustal S-wave Qestimated from MLamplitude I:attenuation in differenttectonic regions of China.Chinese J.Geophys.(in Chinese),2007,50(6):1740-1747.
[13]汪素云,裴顺平,Thomas M H等.利用ML振幅研究地壳横波Q值Ⅱ:Q横向变化特征.地球物理学报,2008,51(1):133-139.Wang S Y,Pei S P,Thomas M H.Crustal S-wave Qestimated from MLamplitudeⅡ:Q lateral variation inChina.Chinese J.Geophys.(in Chinese),2008,51(1):133-139.
[14]周龙泉,刘杰,苏有锦等.利用S波高频衰减参数对云南地区地壳Q值成像.地球物理学报,2009,52(2):1500-1507.Zhou L Q,Liu J,Su Y J,et al.Tomography for Q ofYunnan region from high-frequency attenuation of S wave.Chinese J.Geophys.(in Chinese),2009,52(6):1500-1507.
[15]张杰卿,刘杰,周龙泉.2000年云南姚安地震余震区的速度和衰减结构层析成像分析.地震,2009,29(3):126-135.Zhang J Q,Liu J,Zhou L Q.Tomography and analysis ofvelocity and attenuation structure for the 2000 Yao′anaftershock area in Yunnan.Earthquake(in Chinese),2009,29(3):126-135.
[16]卢显,张晓东,周龙泉等.紫坪铺水库库区地震精定位研究及分析.地震,2010,30(2):10-19.Lu X,Zhang X D,Zhou L Q,et al.Accurate relocation andanalysis of earthquakes in the Zipingpu reservoir area,Sichuan,China.Earthquake(in Chinese),2010,30(2):10-19.
[17]张致伟,程万正,张永久等.汶川8.0级地震前紫坪铺水库小震活动及震源参数研究.中国地震,2009,25(4):367-376.Zhang Z W,Cheng W Z,Zhang Y J,et al.Research onseismicity and source parameters of small earthquakes in theZipingpu dam before Wenchuan Ms8.0earthquake.EarthquakeResearch in China(in Chinese),2009,25(4):367-376.
[18]胡先明,张永久,谢蓉华等.紫坪铺水库区小地震震源机制研究.地震地质,2009,31(4):676-685.Hu X M,Zhang Y J,Xie R H,et al.Research on focalmechanism of small earthquakes in Zipingpu Reservoir Area.Seismology and Geology(in Chinese),2009,31(4):676-685.
[19]雷兴林,马胜利,闻学泽等.地表水体对断层应力与地震时空分布影响的综合分析———以紫坪铺水库为例.地震地质,2008,30(4):1047-1064.Lei X L,Ma S L,Wen X Z,et al.Integrated analysis ofstress and regional seismicity by surface loading—A casestudy of Zipingpu Reservoir.Seismology and Geology(inChinese),2008,30(4):1047-1064.
[20]张永久,赵翠萍.紫坪铺水库库区介质衰减、台站响应和震源参数研究.地震地质,2009,31(4):664-675.Zhang Y J,Zhao C P.Study of attenuation characteristics,site response and seismic source parameters of the ZipingpuReservoir Region.Seismology and Geology(in Chinese),2009,31(4):664-675.
[21]周连庆,赵翠萍,陈章立.紫坪铺水库地区尾波Qc值研究.地震,2009,29(4):44-51.Zhou L Q,Zhao C P,Chen Z L.Coda wave Qcvalues in theZipingpu reservoir area,Sichuan Province.Earthquake(inChinese),2009,29(4):44-51.
[22]周斌.水库诱发地震时空演化特征及其动态响应机制研究—以紫坪铺水库为例[博士论文].北京:中国地震局地质研究所,2010.Zhou B.Evolution characteristics of reservoir-inducedseismicity in space-time and its dynamic response mechanism—Acase study of the Zipingpu Reservoir(in Chinese)[Ph.D.thesis].Beijing:Institute of Geology,China EarthquakeAdministration,2010.
[23]Sherbaum F.Combined inversion for the three-dimensional Qstructure and source parameters using microearthquakespectra.J.Geophys.Res.,1990,95(B8):12423-12438.
[24]Haberland C,Rietbrock A.Attenuation tomography in thewestern central Andes:A detailed insight into the structureof a magmatic arc.J.Geophys.Res.,2001,106(B6):11151-11167.
[25]Brune J N.Tectonic stress and the spectra of seismic shearwaves from earthquakes.J.Geophys.Res.,1970,75(26):4997-5009.
[26]Hanks T C,Wyss M.The use of body-wave spectra in thedetermination of seismic-source parameters.Bull.Seismol.Soc.Am.,1972,62(2):561-589.
[27]Atkinson G M,Mereu R F.The shape of ground motionattenuation curves in southeastern Canada.Bulletin of theSeismological Society of America,1992,82(5):2014-2031.
[28]黄玉龙,郑斯华,刘杰等.广东地区地震动衰减和场地响应的研究.地球物理学报,2003,46(1):54-61.Huang Y L,Zheng S H,Liu J,et al.Attenuation of groundmotion and site response in Guangdong region.Chinese J.Geophys.(in Chinese),2003,46(1):54-61.
[29]苏有锦,刘杰,郑斯华等.云南地区S波非弹性衰减Q值研究.地震学报,2006,28(2):206-212.Su Y J,Liu J,Zheng S H,et al.Qvalue of anelastic S-waveattenuation in Yunnan region.Acta Seismologica Sinica(inChinese),2006,28(2):206-212.
[30]Sherbaum F.Combined inversion for the three-dimensional Qstructure and source parameters using microearthquakespectra.J.Geophys.Res.,1990,95(B8):12423-12438.
[31]Cormier V F.The effect of attenuation on seismic bodywaves.Bull.Seismol.Soc.Am.,1982,72(6B):169-200.
[32]Wittlinger G H,Haessler H,Granet M.Three-dimensionalinversion of Qpfrom low magnitude earthquakes analysis.Ann.Geophys.,1983,1(6):427-438.
[33]刘杰,郑斯华,黄玉龙.利用遗传算法反演非弹性衰减系数、震源参数和场地响应.地震学报,2003,25(2):211-218.Liu J,Zheng S H,Huang Y L.The inversion of non-elasticity coefficient,source parameters,site response usingGenetic algorithms.Acta Seismologica Sinica(in Chinese),2003,25(2):211-218.
[34]安勇,牟永光,方朝亮.沉积岩的速度、衰减与岩石物理性质间的关系.石油地球物理学报,2006,41(2):188-192.An Y,Mu Y G,Fang C L.Relationship betweenattenuation,velocity of sedimentary rocks and petrophysicalproperty.Oil Geophysical Prospecting(in Chinese),2006,41(2):188-192.
[35]李亚林,贺振华,黄德济等.岩石孔渗特性与地震波衰减、传播速度的相互关系.天然气工业,2001,21(4):7-11.Li Y L,He Z H,Huang D J,et al.Relation between rockporosity-permeability property and seismic wave attenuationand propagation velocity.Natural Gas Industry(in Chinese),2001,21(4):7-11.
[36]滕吉文,张中杰,白武明.岩石圈物理学.北京:科学出版社,2004.Teng J W,Zhang Z J,Bai W M.Lithosphere physics(inChinese).Beijing:Science Press,2004.
[37]施行觉,徐果明,靳平等.岩石的含水饱和度对纵、横波速及衰减影响的实验研究.地球物理学报,1995,38(1):281-287.Shi X J,Xu G M,Jin P,et al.The laboratory study ofinfluence of water saturation on rock′s velocity and attenuation.Chinese J.Geophys.(in Chinese),1995,38(1):281-287.
[38]刘斌,Kern H,Popp T.不同围压下孔隙度不同的干燥及水饱和岩样中的纵横波速度及衰减.地球物理学报,1998,41(4):537-546.Liu B,Kern H,Popp T.Velocities and attenuation of P-andS-waves in dry and wet rocks with different porosities underdifferent confining pressures.Chinese J.Geophys.(in Chinese),1998,41(4):537-546.
[39]王云基.四川紫坪铺水库区水文地质与工程地质条件研究.四川地震,2001,(2):6-13.Wang Y J.Hydro-geologic and engineering-geologic conditions ofZipingpureservoir area,Sichuan.Earthquake Research inSichuan(in Chinese),2001,(2):6-13.
[40]李明诚,孙大明.地流体、封隔体和含油气系统与油气运移的关系.石油大学学报:自然科学版,2000,24(4):29-33.Li M C,Sun D M.Relationship of geofluid,compartmentand petroleum system with hydrocarbons migration.Journalof the University of Petroleum,China(in Chinese),2000,24(4):29-33.
[41]赵密福.断层封闭性研究现状.新疆石油地质,2004,25(3):333-336.Zhao M F.A review on fault seal study.Xinjiang PetroleumGeology(in Chinese),2004,25(3):333-336.
[42]刘树根,田小彬,李智武等.龙门山中段构造特征与汶川地震.成都理工大学学报:自然科学版,2008,35(4):388-397.Liu S G,Tian X B,Li Z W,et al.Structural features of thecentral Longmen Mountains and the Wenchuan earthquake inSichuan,China.Journal of Chengdu university of Technology:Science&Technology Edition(in Chinese),2008,35(4):388-397.
[43]郭永刚,常廷改,苏克忠.汶川8.0级特大地震与紫坪铺水库蓄水关系的讨论.震灾防御技术,2008,3(3):259-265.Guo Y G,Chang T G,Su K Z.Discussion on relationbetween water recharge of Zipuping reservoir and WenchuanMs8.0 Earthquake.Technology for Earthquake DisasterPrevention(in Chinese),2008,3(3):259-265.
[44]王伟君,陈凌,陈棋福等.2003年大姚地震震中区的速度和衰减结构.地球物理学报,2007,50(3):116-125.Wang W J,Chen L,Chen Q F,et al.Velocity andattenuation structures in the focal area of 2003 Dayaoearthquakes.Chinese J.Geophys.(in Chinese),2007,50(3):116-125.
[45]Eberhart-Phillips D,Chadwick M.Three-dimensional attenuationmodel of the shallow Hikurangi subduction zone in theRaukumara Peninsula,New Zealand.J.Geophys.Res.,2002,107:2033,doi:10.1029/2000JB000046.
[2]王大兴,辛可锋,李幼铭等.地层条件下砂岩含水饱和度对波速及衰减影响的实验研究.地球物理学报,2006,49(3):908-914.Wang D X,Xin K F,Li Y M,et al.An experimental studyof influence of water saturation on velocity and attenuation insandstone under stratum conditions.Chinese J.Geophys.(inChinese),2006,49(3):908-914.
[3]刘建华,胥颐,郝天珧.地震波衰减的物理机制研究.地球物理学进展,2004,19(1):1-7.Liu J H,Xu Y,Hao T Y.Study on physical mechanism ofthe seismic wave attenuation.Progress in Geophysics(inChinese),2004,19(1):1-7.
[4]Sato Y.Attenuation,dispersion,and the wave guide of the Gwave.Bull.Seism.Soc.Am.,1958,48(3):231-251.
[5]Anderson D L,Archambeau C B.The anelasticity of theearth.J.Geophys.Res.,1964,69(10):2071-2084.
[6]Haydar J,AI-Shukri H K,Mitchell B J.Three-dimensionalattenuation structure in and around the new Madrid seismiczone.Bull.Seism.Soc.Ain.,l990,80(3):615-632.
[7]Hansen S,Thurber C,Mandernach M,et al.Seismicvelocity and attenuation structure of the east rift zone andsouth Flank of Kilauea volcano,Hawaii.Bulletin of theSeismological Society of America,2004,94(4):1430-1440.
[8]丛连理,胡家富,傅竹武等.中国大陆及邻近地区Lg尾波的Q值分布.中国科学(D辑),2002,32(8):617-624.Cong L L,Hu J F,Fu Z W,et al.Distribution Lg coda Q-value in China and its neighboring regions.Science in China(Series D)(in Chinese),2002,32(8):617-624.
[9]洪学海,朱介寿,曹家敏等.中国大陆地壳上地幔S波品质因子三维层析成像.地球物理学报,2003,46(5):642-651.Hong X H,Zhu J S,Cao J M,et al.Tomography of the 3-DS-wave quality factor of the crust and upper mantle in China.Chinese J.Geophys.(in Chinese),2003,46(5):642-651.
[10]Pei S P,Zhan J M,Rowe C A,et al.MLamplitudetomography in North China.Bull.Seismo.Soc.Am.,2006,96(4A):1560-1566.
[11]马宏生,汪素云,裴顺平等.川滇及周边地区地壳横波衰减的成像研究.地球物理学报,2007,50(2):465-471.Ma H S,Wang S Y,Pei S P,et al.Q0tomography of S waveattenuation in Sichuan-yunnan and adjacent regions.ChineseJ.Geophys.(in Chinese),2007,50(2):465-471.
[12]汪素云,裴顺平,许忠淮等.利用ML振幅研究地壳横波Q值I:不同构造区的衰减特征.地球物理学报,2007,50(6):1740-1747.Wang S Y,Pei S P,Xu Z H,et al.Crustal S-wave Qestimated from MLamplitude I:attenuation in differenttectonic regions of China.Chinese J.Geophys.(in Chinese),2007,50(6):1740-1747.
[13]汪素云,裴顺平,Thomas M H等.利用ML振幅研究地壳横波Q值Ⅱ:Q横向变化特征.地球物理学报,2008,51(1):133-139.Wang S Y,Pei S P,Thomas M H.Crustal S-wave Qestimated from MLamplitudeⅡ:Q lateral variation inChina.Chinese J.Geophys.(in Chinese),2008,51(1):133-139.
[14]周龙泉,刘杰,苏有锦等.利用S波高频衰减参数对云南地区地壳Q值成像.地球物理学报,2009,52(2):1500-1507.Zhou L Q,Liu J,Su Y J,et al.Tomography for Q ofYunnan region from high-frequency attenuation of S wave.Chinese J.Geophys.(in Chinese),2009,52(6):1500-1507.
[15]张杰卿,刘杰,周龙泉.2000年云南姚安地震余震区的速度和衰减结构层析成像分析.地震,2009,29(3):126-135.Zhang J Q,Liu J,Zhou L Q.Tomography and analysis ofvelocity and attenuation structure for the 2000 Yao′anaftershock area in Yunnan.Earthquake(in Chinese),2009,29(3):126-135.
[16]卢显,张晓东,周龙泉等.紫坪铺水库库区地震精定位研究及分析.地震,2010,30(2):10-19.Lu X,Zhang X D,Zhou L Q,et al.Accurate relocation andanalysis of earthquakes in the Zipingpu reservoir area,Sichuan,China.Earthquake(in Chinese),2010,30(2):10-19.
[17]张致伟,程万正,张永久等.汶川8.0级地震前紫坪铺水库小震活动及震源参数研究.中国地震,2009,25(4):367-376.Zhang Z W,Cheng W Z,Zhang Y J,et al.Research onseismicity and source parameters of small earthquakes in theZipingpu dam before Wenchuan Ms8.0earthquake.EarthquakeResearch in China(in Chinese),2009,25(4):367-376.
[18]胡先明,张永久,谢蓉华等.紫坪铺水库区小地震震源机制研究.地震地质,2009,31(4):676-685.Hu X M,Zhang Y J,Xie R H,et al.Research on focalmechanism of small earthquakes in Zipingpu Reservoir Area.Seismology and Geology(in Chinese),2009,31(4):676-685.
[19]雷兴林,马胜利,闻学泽等.地表水体对断层应力与地震时空分布影响的综合分析———以紫坪铺水库为例.地震地质,2008,30(4):1047-1064.Lei X L,Ma S L,Wen X Z,et al.Integrated analysis ofstress and regional seismicity by surface loading—A casestudy of Zipingpu Reservoir.Seismology and Geology(inChinese),2008,30(4):1047-1064.
[20]张永久,赵翠萍.紫坪铺水库库区介质衰减、台站响应和震源参数研究.地震地质,2009,31(4):664-675.Zhang Y J,Zhao C P.Study of attenuation characteristics,site response and seismic source parameters of the ZipingpuReservoir Region.Seismology and Geology(in Chinese),2009,31(4):664-675.
[21]周连庆,赵翠萍,陈章立.紫坪铺水库地区尾波Qc值研究.地震,2009,29(4):44-51.Zhou L Q,Zhao C P,Chen Z L.Coda wave Qcvalues in theZipingpu reservoir area,Sichuan Province.Earthquake(inChinese),2009,29(4):44-51.
[22]周斌.水库诱发地震时空演化特征及其动态响应机制研究—以紫坪铺水库为例[博士论文].北京:中国地震局地质研究所,2010.Zhou B.Evolution characteristics of reservoir-inducedseismicity in space-time and its dynamic response mechanism—Acase study of the Zipingpu Reservoir(in Chinese)[Ph.D.thesis].Beijing:Institute of Geology,China EarthquakeAdministration,2010.
[23]Sherbaum F.Combined inversion for the three-dimensional Qstructure and source parameters using microearthquakespectra.J.Geophys.Res.,1990,95(B8):12423-12438.
[24]Haberland C,Rietbrock A.Attenuation tomography in thewestern central Andes:A detailed insight into the structureof a magmatic arc.J.Geophys.Res.,2001,106(B6):11151-11167.
[25]Brune J N.Tectonic stress and the spectra of seismic shearwaves from earthquakes.J.Geophys.Res.,1970,75(26):4997-5009.
[26]Hanks T C,Wyss M.The use of body-wave spectra in thedetermination of seismic-source parameters.Bull.Seismol.Soc.Am.,1972,62(2):561-589.
[27]Atkinson G M,Mereu R F.The shape of ground motionattenuation curves in southeastern Canada.Bulletin of theSeismological Society of America,1992,82(5):2014-2031.
[28]黄玉龙,郑斯华,刘杰等.广东地区地震动衰减和场地响应的研究.地球物理学报,2003,46(1):54-61.Huang Y L,Zheng S H,Liu J,et al.Attenuation of groundmotion and site response in Guangdong region.Chinese J.Geophys.(in Chinese),2003,46(1):54-61.
[29]苏有锦,刘杰,郑斯华等.云南地区S波非弹性衰减Q值研究.地震学报,2006,28(2):206-212.Su Y J,Liu J,Zheng S H,et al.Qvalue of anelastic S-waveattenuation in Yunnan region.Acta Seismologica Sinica(inChinese),2006,28(2):206-212.
[30]Sherbaum F.Combined inversion for the three-dimensional Qstructure and source parameters using microearthquakespectra.J.Geophys.Res.,1990,95(B8):12423-12438.
[31]Cormier V F.The effect of attenuation on seismic bodywaves.Bull.Seismol.Soc.Am.,1982,72(6B):169-200.
[32]Wittlinger G H,Haessler H,Granet M.Three-dimensionalinversion of Qpfrom low magnitude earthquakes analysis.Ann.Geophys.,1983,1(6):427-438.
[33]刘杰,郑斯华,黄玉龙.利用遗传算法反演非弹性衰减系数、震源参数和场地响应.地震学报,2003,25(2):211-218.Liu J,Zheng S H,Huang Y L.The inversion of non-elasticity coefficient,source parameters,site response usingGenetic algorithms.Acta Seismologica Sinica(in Chinese),2003,25(2):211-218.
[34]安勇,牟永光,方朝亮.沉积岩的速度、衰减与岩石物理性质间的关系.石油地球物理学报,2006,41(2):188-192.An Y,Mu Y G,Fang C L.Relationship betweenattenuation,velocity of sedimentary rocks and petrophysicalproperty.Oil Geophysical Prospecting(in Chinese),2006,41(2):188-192.
[35]李亚林,贺振华,黄德济等.岩石孔渗特性与地震波衰减、传播速度的相互关系.天然气工业,2001,21(4):7-11.Li Y L,He Z H,Huang D J,et al.Relation between rockporosity-permeability property and seismic wave attenuationand propagation velocity.Natural Gas Industry(in Chinese),2001,21(4):7-11.
[36]滕吉文,张中杰,白武明.岩石圈物理学.北京:科学出版社,2004.Teng J W,Zhang Z J,Bai W M.Lithosphere physics(inChinese).Beijing:Science Press,2004.
[37]施行觉,徐果明,靳平等.岩石的含水饱和度对纵、横波速及衰减影响的实验研究.地球物理学报,1995,38(1):281-287.Shi X J,Xu G M,Jin P,et al.The laboratory study ofinfluence of water saturation on rock′s velocity and attenuation.Chinese J.Geophys.(in Chinese),1995,38(1):281-287.
[38]刘斌,Kern H,Popp T.不同围压下孔隙度不同的干燥及水饱和岩样中的纵横波速度及衰减.地球物理学报,1998,41(4):537-546.Liu B,Kern H,Popp T.Velocities and attenuation of P-andS-waves in dry and wet rocks with different porosities underdifferent confining pressures.Chinese J.Geophys.(in Chinese),1998,41(4):537-546.
[39]王云基.四川紫坪铺水库区水文地质与工程地质条件研究.四川地震,2001,(2):6-13.Wang Y J.Hydro-geologic and engineering-geologic conditions ofZipingpureservoir area,Sichuan.Earthquake Research inSichuan(in Chinese),2001,(2):6-13.
[40]李明诚,孙大明.地流体、封隔体和含油气系统与油气运移的关系.石油大学学报:自然科学版,2000,24(4):29-33.Li M C,Sun D M.Relationship of geofluid,compartmentand petroleum system with hydrocarbons migration.Journalof the University of Petroleum,China(in Chinese),2000,24(4):29-33.
[41]赵密福.断层封闭性研究现状.新疆石油地质,2004,25(3):333-336.Zhao M F.A review on fault seal study.Xinjiang PetroleumGeology(in Chinese),2004,25(3):333-336.
[42]刘树根,田小彬,李智武等.龙门山中段构造特征与汶川地震.成都理工大学学报:自然科学版,2008,35(4):388-397.Liu S G,Tian X B,Li Z W,et al.Structural features of thecentral Longmen Mountains and the Wenchuan earthquake inSichuan,China.Journal of Chengdu university of Technology:Science&Technology Edition(in Chinese),2008,35(4):388-397.
[43]郭永刚,常廷改,苏克忠.汶川8.0级特大地震与紫坪铺水库蓄水关系的讨论.震灾防御技术,2008,3(3):259-265.Guo Y G,Chang T G,Su K Z.Discussion on relationbetween water recharge of Zipuping reservoir and WenchuanMs8.0 Earthquake.Technology for Earthquake DisasterPrevention(in Chinese),2008,3(3):259-265.
[44]王伟君,陈凌,陈棋福等.2003年大姚地震震中区的速度和衰减结构.地球物理学报,2007,50(3):116-125.Wang W J,Chen L,Chen Q F,et al.Velocity andattenuation structures in the focal area of 2003 Dayaoearthquakes.Chinese J.Geophys.(in Chinese),2007,50(3):116-125.
[45]Eberhart-Phillips D,Chadwick M.Three-dimensional attenuationmodel of the shallow Hikurangi subduction zone in theRaukumara Peninsula,New Zealand.J.Geophys.Res.,2002,107:2033,doi:10.1029/2000JB000046.
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