引文
[1]费琪.第四届全国构造会议报告.北京,2008,10.
[1]Qiu Ning,Zeng Zuoxun,Yang Yichun.Design of Monitoring and Early Warning Systemfor Geological Hazardsin Three Gor-ges Reservoir Area UsingInfrasound,2008Infrasound Technol-ogy Workshop Bermuda.2008.
[2]曾佐勋,强祖基,刘江平,等.地气、动物行为异常与地震短临预测系统.第四届全国构造会议论文摘要集.北京,2008:564-565.
[1]Xu Z H.A present-day tectonic stress map for eastern Asia region[J].Acta Seismologica Sinica,2001,23(5):492-501(in Chinese).
[2]Zhao D P,Akira Y,Yuhei O.Precisely measured travel ti mes of mantle body waves:I mplications for mantle hetero-geneity and tomography[J].Earth Science Frontiers,2006,13(2):37-47.
[3]Luo WX,Li D W,Wang X F.Focal depth and mechanismof intraplate earthquakes in the Qinghai-Tibet Plateau[J].Earth Science—Journal of China University of Geosciences,2008,33(5):618-626(in Chinese).
[4]Zang S X,Yang J L.Distribution of focal depths for intraplateearthquakesin North China andits physical explanation[J].Seis-mology and Geology,1984,6(3):67-76(in Chinese).
[5]Sykes L R,Sbar M L.Intraplate earthquakes,lithospheric stresses and the driving mechanismof plate tectonics[J].Na-ture,1973,245:298-302(in Chinese).
[6]Zhang Z M.Correlation between in traplate earthquake and plate margin earthquake in China and adjacent area[J].Seis-mology and Geology,1979,1(3):12-23(in Chinese).
[7]Li D W.The style of continental structure and model of con-tinental dynamics[J].Advances in Earth Science,1993,8(5):88-93(in Chinese).
[8]Zhao Y G,Zhong D L,Liu J H,et al.Fundamentals of geo-logical interpretation for seismic tomography and its applica-tion to studying of west Yunnan s deep structure[J].Scientia Geologica Sinica,1992(2):105-113(in Chinese).
[9]Ma Z J.Current state of research on continental seismogenic layer[J].Seismology and Geology,1990,12(3):262-264(in Chinese).
[10]Liu F T,Qu K X,Wu H,et al.STi mage of North China[J].Journal of Geophysics,1986,29:442-449(in Chinese).
[11]Liu J H,Wu H,Liu F T,et al.Features of3-Dvelocity dis-tribution andlithosphere structurein South China andits con-tiguous sea area[J].Chinese Journal of Geophysics,1996,39:483-492(in Chinese).
[12]Friederich W.The S-velocity structure of the East Asian mantle frominversion of shear and surface waveforms[J].Geophys J Int,2003,153:88-102.
[13]Zhu J S,Gao J M,Cai X L,et al.Studyfor three-di mension-al structure of Earth interior and geodynamics in China and adjacent land and sea regions[J].Advances in Earth Science,2003,18(4):497-503(in Chinese).
[14]Q C,Zhao D,Chen Y,et al.3-D P and S wave velocity structures and their relationship to strong earthquakes in the Chinese capital region[J].Chinese J Geophys,2006,49(3):805-815(in Chinese).
[15]He R,Zhao D,Gao R,et al.Teleseismic P-wave tomo-graphy of lithospheric mantle beneath west Kunlun orogenic belts[J].Chinese J Geophys,2006,49(3):778-787(in Chi-nese).
[16]Cai X L,Zhu J S,Gao J M,et al.Three di mensional tecton-ics of lithosphere and mantle dynamics of East Asia-West Pa-cific[J].Earth Science Frontiers,2007,14(3):21-38(in Chi-nese).
[17]Xing Z Y,Xing J S,Zhao B,et al.Identification of deep structure of two episodes in North China and its signifi-cance—Yanshanian Movement and deep process[J].Geolog-ical Review,2006,52(4):433-441(in Chinese).
[18]Xing J S,Yang WR,Xing Z Y,et al.Deep-seated structure characteristics of Eastern China and its relation with metalmineralization-concentrated region[J].Earth Science Fron-tiers,2007,14(3):114-130(in Chinese).
[19]Qiang Z J,Xu X D,Dian C G.Thermal infrared anomaly precursor of i mpending earthquakes[J].Pure and Applied Geophysics,1997,149(1):159-171.
[20]Yang WR.Earth surface systemand research history of the regional geotectonics of China[J].Earth Science Frontiers,2006,13(6):102-110(in Chinese).
[21]Xu C F.The cause of formation of the upper mantle and crust high conductive layers in Chinese mainland and the study of Tangshan earthquake[J].Earth Science Frontiers,2003,10(Suppl):101-111(in Chinese).
[22]Xing Z Y,Zhao B,Tu MY,et al.The formation of the Fen-wei rift valley[J].Earth Science Frontiers,2005,12(2):247-262(in Chinese).
[23]Yang WR,Sun J Y,Ji K C,et al.Comparisonfor Continen-tal Rifts:Analysis of the Fenwei and Baikal Rift Systems[M].Wuhan:China University of Geosciences Press,1995:1-127(in Chinese).
[1]许忠淮.东亚地区现今构造应力图的编制[J].地震学报,2001,23(5):492-501.
[3]罗文行,李德威,汪校锋.青藏高原板内地震震源深度分布规律及其成因[J].地球科学——中国地质大学学报,2008,33(5):618-626.
[4]臧绍先,杨君亮.我国华北等地区板内地震的深度分布及其物理背景[J].地震地质,1984,6(3):67-76.
[6]张之孟.我国及邻区板内地震与板缘地震的关系[J].地震地质,1979,1(3):12-23.
[7]李德威.大陆构造样式及大陆动力学模式初探[J].地球科学进展,1993,8(5):88-93.
[8]赵永贵,钟大赉,刘建华,等.地震层析地质解释原理及其在滇西深部构造研究中的应用[J].地质科学,1992(2):105-113.
[9]马宗晋.大陆多震层研究现状和讨论[J].地震地质,1990,12(3):262-264.
[10]刘福田,曲克信,吴华,等.华北地区的地震层面成像[J].地球物理学报,1986,29:442-449.
[11]刘建华,吴华,刘福田.华南及其海域三维速度分布特征与岩石层结构[J].地球物理学报,1996,39:483-492.
[13]朱介寿,曹家敏,蔡学林,等.中国及邻近海域地球内部三维结构及动力学研究[J].地球科学进展,2003,18(4):497-503.
[14]齐诚,赵大鹏,陈顒,等.首都圈地区地壳P波和S波三维速度结构及其与大地震关系[J].地球物理学报,2006,49(3):805-815.
[15]贺日政,赵大鹏,高锐,等.利用远震P波层析成像研究西昆仑造山带下岩石圈地幔速度结构[J].地球物理学报,2006,49(3):778-787.
[16]蔡学林,朱介寿,曹家敏,等.东亚太平洋岩石圈三维结构及其地幔动力学[J].地学前缘,2007,14(3):21-38.
[17]邢作云,邢集善,赵斌,等.华北地区两个世代深部构造的识别及其意义——燕山运动与深部过程[J].地质论评,2006,52(4):433-441.
[18]邢集善,杨巍然,邢作云,等.中国东部深部构造特征及其与矿集区关系[J].地学前缘,2007,14(3):114-130.
[20]杨巍然.地球表层系统与中国区域大地构造的研究发展[J].地学前缘,2006,13(6):102-110.
[21]徐常芳.中国大陆壳内与上地幔高导层成因及唐山地震机理研究[J].地学前缘,2003,10(特刊):101-111.
[22]邢作云,赵斌,涂美义,等.汾渭裂谷系与造山带耦合关系及其形成机制研究[J].地学前缘,2005,12(2):247-262.
[23]杨巍然,孙继源,纪克诚,等.大陆裂谷对比——汾渭裂谷与贝加尔裂谷系例析[M].武汉:中国地质大学出版社,1995:1-127.