引文
[1]丁原章.水库诱发地震.北京:地震出版社,1989:11-20,26-36,64-80.Ding Y Z.The Reservoir Induced Earthquake(in Chinese).Beijing:Seismological Press,1989:11-20,26-36,64-80.
[2]丁原章,潘建雄,肖安予等.新丰江水库诱发地震的构造条件.地震地质,1983,5(3):63-74.Ding Y Z,Pan J X,Xiao A Y,et al.Tectonic environment ofreservoir induced earthquake in the Xinfengjiang reservoirarea.Seismology and Geology(in Chinese),1983,5(3):63-74.
[3]潘建雄,肖安予.新丰江水库区地震构造及其活动特征的初步研究.地震地质,1982,4(2):53-58.Pan J X,Xiao A Y.The preliminary study of seismicstructures and their characteristic activity in Xinfengjiangreservoir area.Seismology and Geology(in Chinese),1982,4(2):53-58.
[4]王妙月,杨懋源,胡毓良等.新丰江水库地震的震源机制及其成因的初步探讨.中国科学(A辑),1976,(1):85-97.Wang M Y,Yang M Y,Hu Y L,et al.A preliminary studyon the mechanism of the reservoir impounding earthquakes atHsinfengkiang.Science in China,Ser.A(in Chinese),1976,(1):85-97.
[5]陈益明.新丰江水库地震及其小震震源机制的研究.华南地震,1982,2(3):64-71.Chen Y M.The focal mechanism study of Xinfengjiangreservoir-induced earthquakes and its micro aftershocks.South China Journal of Seismology(in Chinese),1982,2(3):64-71.
[6]丁原章,曾宪译,陈益明.新丰江水库区诱发地震的余震活动.地震地质,1982,4(1):23-29.Ding Y Z,Zeng X Y,Chen Y M.The aftershock activities ofinduced earthquakes in the Xinfengjiang reservoir areas.Seismology and Geology(in Chinese),1982,4(1):23-29.
[7]中国科学院地质研究所破裂与震源力学组,广东省科技局新丰江地震总结组.新丰江水库区微震震源力学的初步研究.地质科学,1974,(3):234-245.Focal mechanism and fracture researching group,Institute ofGeology,Academia Sinica,Hsinfengkiang earthquakesresearching group,Kwangtung Scientific and TechnologicalDepartment.A preliminary analysis of the mechanism ofmicroearthquakes in the region of Hsinfengkiang reservoir.Scientia Geologica Sinica(in Chinese),1974,(3):234-245.
[8]臧绍先.水的渗透作用及新丰江水库地震的特点和机制.地震地质,1983,5(2):59-69.Zang S X.The effect of infiltrating of water and mechanismand characteristics of earthquakes in Xinfengjiang reservoir.Seismology and Geology(in Chinese),1983,5(2):59-69.
[9]沈立英.渗流与新丰江水库地震.华南地震,1989,9(2):92-101.Shen L Y.The influent and earthquakes in Xinfengjiangreservoir.South China Journal of Seismology(in Chinese),1989,9(2):92-101.
[10]魏柏林,陈庞龙,李富光等.新丰江地震震源机制解及构造应力场.地震学报,1991,13(4):462-479.Wei B L,Chen P L,Li F G,et al.Focal mechanisms andtectonic stress field of the Xinfengjiang earthquakes.ActaSeismologica Sinica(in Chinese),1991,13(4):462-479.
[11]丁原章,王仁,孙荀英等.深层构造新活动性的影响——新丰江水库区构造的三维数学模拟计算.中国科学(B辑),1992,(2):194-205.Ding Y Z,Wang R,Sun X Y,et al.Influence of the deepstructure new activity—three-dimensional mathematicalsimulation of the tectonics in Xinfengjiang reservoir area.Science in China,Ser.B(in Chinese),1992,(2):194-205.
[12]胡毓良,陈献程.我国的水库地震及有关成因问题的讨论.地震地质,1979,1(4):45-57.Hu Y L,Chen X C.Discussion on the reservoir-inducedearthquakes in China and some problems related to theirorigin.Seismology and Geology(in Chinese),1979,1(4):45-57.
[13]李安然,徐永键,韩晓光等.中国东部四个水库震例的诱震环境因素研究.华南地震,1990,10(3):89-99.Li A R,Xu Y J,Han X G,et al.Environment factors ofinduced earthquake of four reservoirs in eastern China.SouthChina Journal of Seismology(in Chinese),1990,10(3):89-99.
[14]黄腾浪,杨马陵.新丰江地震S波偏振的初步研究.华南地震,2001,21(4):22-26.Huang T L,Yang M L.Preliminary study on polarization ofS-wave of Xinfengjiang earthquakes.South China Journal ofSeismology(in Chinese),2001,21(4):22-26.
[15]官幼雄,李亚林,颜玉定.1962年3月19日新丰江6.1级水库诱发地震时的构造应力.华南地震,2005,25(3):83-86.Gong Y X,Li Y L,Yan Y D.A study on the tectonic stressvariation caused by Xinfengjiang Ms6.1reservoir inducedearthquake occured on March 19,1962.South China Journalof Seismology(in Chinese),2005,25(3):83-86.
[16]万永芳,叶东华,陈大庆.广东新丰江地区地震研究.华南地震,2008,28(2):60-66.Wan Y F,Ye D H,Chen D Q.Study on earthquakecharacteristics in Xinfengjiang region.South China Journalof Seismology(in Chinese),2008,28(2):60-66.
[17]吴建春,冯锐,宋仲和.CT技术在新丰江台网中的应用.中国地震,1990,6(4):85-92.Wu J C,Feng R,Song Z H.Application of ComputerizedTomography on the Xinfengjiang Reservoir Network.Earthquake Research in China(in Chinese),1990,6(4):85-92.
[18]郭贵安,冯锐.新丰江水库三维速度结构和震源参数的联合反演.地球物理学报,1992,35(3):331-342.Guo G A,Feng R.The joint inversion of 3-D velocitystructure and source parameters in Xinfengjiang reservoir.Chinese Journal of Geophysics(in Chinese),1992,35(3):331-342.
[19]Tarantola A,Nercessian A.Three-dimensional inversionwithout blocks.Geophys.J.R.Astr.Soc,1984,76:299-306.
[20]张先康,杨卓欣,杨玉春等.地壳三维结构的层析成像方法—爆炸和地震资料的联合反演.地震学报,1995,17(4):422-431.Zhang X K,Yang Z X,Yang Y C,et al.Method oftomographic determination of the 3-D crustal structure:Jointinversion of explosion and earthquake data.Acta SeismologicaSinica(in Chinese),1995,17(4):422-431.
[21]王洪体,庄灿涛,薛兵等.精密主动地震监测.地球物理学报,2009,52(7):1808-1815.Wang H T,Zhuang C T,Xue B,et al.Precisely and activelyseismic monitoring.Chinese Journal of Geophysics(inChinese),2009,52(7):1808-1815.
[22]Nercessian A,Hirn A,Tarantola A.Three-dimensionalseismic transmission prospecting of the Mont Dore volcano,France.Geophys.J.R.Astr.Soc,1984,76:307-315.
[23]Tarantola A.Inverse Problem Theory:Methods for DataFitting and Model Parameter Estimation.New York:Elsevier Science Publ.Co.,1986:506-528.
[24]张先康,杨玉春,赵平等.唐山滦县震区的三维地震透射研究——中、上地壳速度层析成像.地球物理学报,1994,37(6):687-694.Zhang X K,Yang Y C,Zhao P,et al.Three-dimensionalseismic transmission experiment in the Luanxian earthquakeregion of North China:tomographic determination of theupper and middle crust structure.Chinese Journal ofGeophysics(in Chinese),1994,37(6):687-694.
[25]Zelt C A.Lateral velocity resolution from 3-D seismicrefraction data.Geophys.J.Int.,1998,135:1101-1112.
[26]王夫运,张先康,陈棋福等.北京地区上地壳三维细结构层析成像.地球物理学报,2005,48(2):359-366.Wang F Y,Zhang X K,Chen Q F,et al.Fine tomographicinversion of the upper crust 3-D structure around Beijing.Chinese Journal of Geophysics(in Chinese),2005,48(2):359-366.
[27]刘志,张先康,周雪松等.帕米尔东北侧地壳物性结构及其发震环境探讨.地震学报,2003,25(3):242-249.Lu Z,Zhang X K,Zhou X S,et al.Study of crustalstructure in terms of physical property and discussion onseismogenic environment in the northeastern Pamirs.ActaSeismologica Sinica(in Chinese),2003,25(3):242-249.
[28]刘志,张先康,潘纪顺等.阿尼玛卿缝合带及两侧上地壳泊松比分布.地球物理学进展,2009,24(5):1627-1635.Lu Z,Zhang X K,Pan J S,et al.Poisson′s ratio distributionin the upper crust around the A′nyemaqên suture zone and itsadjacent areas.Progress in Geophysics(in Chinese),2009,24(5):1627-1635.
[29]Haggag H M,Bhattacharya P M,Kamal S,et al.Seismicityand 3Dvelocity structure in the Aswan Reservoir Lake area,Egypt.Tectonophysics,2009,476(3-4):450-459.
[30]Talwani P,Acress S.Pore pressure diffusion and themechanism of reservoir induced seismicity.Pure Appl.Geophys.,1985,122:947-955.
[31]Talwani P.Speculation on the causes of continuing seismicitynear Koyna Reservoir,India.Pageoph.,1995,145(1):167-174.
[32]Singh,Chandrani,Ramana D V,et al.Coseismic responsesand the mechanism behind the Mw5.1earthquake of March14,2005in the Koyna-Warna region,India.J.Asian EarthSci.,2008,39:499-513.
[33]易立新,王广才,李榴芬.水文地质结构与水库诱发地震.水文地质工程地质,2004,31(2):29-32.Yi L X,Wang G C,Li L F.Hydrogeological structure andreservoir induced seismicity.Hydrogeology and EngineeringGeology(in Chinese),2004,31(2):29-32.