引文
[1]嘉世旭,张先康,方盛明.华北裂陷盆地不同块体地壳结构及演化研究.地学前缘,2001,8(2):259-266.Jia S X,Zhang X K,Fang S M.Research on the crustalstructure and evolution of different blocks in North China rift-depression basin.Earth Science Frontiers,(in Chinese),2001,8(2):259-266.
[2]张学民.剪切波速度结构研究方法综述.地球物理学进展,2005,20(1):135-141.Zhang X M.The general statement on shear wave velocitystructure research methods.Progress in Geophysics,(inChinese),2005,20(1):135-141.
[3]Zhao D P,Hasegawa A,Kanamori H.Deep structure of Japansubduction zone as derived from local,regional,andteleseismic events.J.Geophys.Res.,1994,99(B11):22313-22329.
[4]房立华,吴建平,吕作勇.华北地区基于噪声的瑞利面波群速度层析成像.地球物理学报,2009,52(3):663-671.Fang L H,Wu J P,LüZ Y.Rayleigh wave group velocitytomography from ambient seismic noise in North China.Chinese J.Geophys.(in Chinese),2009,52(3):663-671.
[5]Zhao D P,Hasegawa A,Horiuchi S.Tomographic imaging ofP and S wave velocity structure beneath northeastern Japan.J.Geophys.Res.,1992,97(B13):19909-19928.
[6]Zheng T Y,Zhao L,Chen L.A detailed receiver function image ofthe sedimentary structure in the Bohai Bay Basin.Phys.EarthPlanet.Inter.,2005,152(3):129-143.
[7]杜金虎,邹伟宏,费宝生等.冀中拗陷古潜山复式油气聚集区.北京:科学出版社,2002.Du J H,Zou W H,Fei B S,et al.Buried Hill CompoundAccumulation Area of Oil and Aas in Jizhong Depression(inChinese).Beijing:Science Press,2002.
[8]马杏垣.中国岩石圈动力学地图集.北京:中国地图出版社,1989.Ma X Y.Lithospheric Dynamics Atlas of China(in Chinese).Beijing:China Cartographic Publishing House,1989.
[9]于湘伟,陈运泰,王培德.京津唐地区中上地壳三维P波速度结构.地震学报,2003,25(1):1-14.YU X W,Chen Y T,Wang P D.Three-dimensional P wavevelocity structure in Beijing-Tianjin-Tangshan area.ActaSeismologica Sinica(in Chinese),2003,25(1):1-14.
[10]王未来,吴建平,房立华.唐海—商都地震台阵剖面下方的地壳上地幔S波速度结构研究.地球物理学报,2009,52(1):81-89.Wang W L,Wu J P,Fang L H.Crust and upper mantle S-wave velocity structure beneath Tanghai-Shangdu seismicarray profile.Chinese J.Geophys.(in Chinese),2009,52(1):81-89.
[11]刘国栋,史书林,王宝钧.华北地区壳内高导层及其与地壳构造活动性的关系.中国科学(B辑),1984,(9):839-848.Liu G D,Shi S L,Wang B J.The relationship between highconductive and crustal tectonic activity in North China.Science China Series B-Chemistry(in Chinese),1984,(9):839-848.
[12]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.地学前缘,2003,10(增):101-111.Xu C F.The cause of formation of the upper mantle and crusthigh conductive layers in Chinese mainland and the study ofTangshan earthquake.Earth Science Frontiers(in Chinese),2003,10(Suppl.):101-111.
[13]陈国英,宋仲和,安昌强等.华北地区三维地壳上地幔结构.地球物理学报,1991,34(2):172-181.Chen G Y,Song Z H,An C Q,et al.Three-dimensionalcrust and upper mantle structure of the North China region.Chinese J.Geophys.(in Chinese),1991,34(2):172-181.
[14]刘国栋.华北平原新生代裂谷系及其深部过程.//国家地震局研究所编.现代地壳运动研究.北京:地震出版社,1985.Liu G D.Cenozoic rift system and the deep process in NorthChina plain.//Institute of National Earthquake Administrationed.The Study on Modern Crustal Movement(in Chinese).Beijing:Seismological Press,1985.
[15]汪洋.中国大陆大地热流分析.北京:中国科学院地质研究所,1999.Wang Y.An analysis for the continental heat flow in China(in Chinese).Beijing:Institute of Geology,ChineseAcademy of Sciences,1999.
[16]秦馨菱,Pedersen L B,赵玉林等.唐山地震区地壳电性结构及MT探索潜在震源的可能性.地震学报,1991,13(3):354-363.Qin X L,Pederson L B,Zhao Y L,et al.Conductivitystructure of crust in the Tangshan seismic area and thepossibility of exploring potential seismic sources bymagnetotelluric method.Acta Seismologica Sinica(inChinese),1991,13(3):354-363.
[17]裴顺平,许忠淮,汪素云.中国大陆及邻近地区上地幔顶部Sn波速度层析成像.地球物理学报,2004,47(2):250-256.Pei S P,Xu Z H,Wang S Y.Sn wave tomography in theuppermost mantle beneath the China continent and adjacentregions.Chinese J.Geophys.(in Chinese),2004,47(2):250-256.
[18]Jackson I,Rigden S M.Composition and temperature of theearth’s mantle:Seismological models interpreted throughexperimental studies of earth materials.//Jackson I ed.TheEarth’s Mantle:Structure,Composition,and Evolution.Cambridge:Cambridge University Press,1998.
[19]Goes S,Govers R,Vacher P.Shallow mantle temperaturesunder Europe from P and S wave tomography.J.Geophys.Res.,2000,105(B5):11153-11169.
[20]刘建华,胥颐,郝天珧等.中国边缘海及邻区地壳和上地幔速度结构特征.地球物理学进展,2005,20(3):594-599.Liu J H,Xu Y,Hao T Y,et al.Three dimensional velocitystructure feature in the crust and upper mantle beneathChinese marginal seas and adjacent regions.Progress inGeophysics(in Chinese),2005,20(3):594-599.
[21]吕作勇,吴建平.华北地区地壳上地幔三维P波速度结构.地震学报,2010,32(1):1-11.LüZ Y,Wu J P.3-D P wave velocity structure of crust andupper mantle beneath North China.Acta Seismologica Sinica(in Chinese),2010,32(1):1-11.
[22]朱露培,曾融生,刘福田.京津唐张地区地壳上地幔三维P波速度结构.地球物理学报,1990,33(3):267-277.Zhu L P,Zeng R S,Liu F T.Three-dimensional P-wavevelocity structure under the Beijing network area.Chinese J.Geophys.(in Chinese),1990,33(3):267-277.
[23]Huang J L,Zhao D P.Crustal heterogeneity and seismotectonicsof the region around Beijing,China.Tectonophysics,2004,385(1-4):159-180.
[24]杨峰,黄金莉,杨挺.应用远震有限频率层析成像反演首都圈上地幔速度结构.地球物理学报,2010,53(8):1806-1816.Yang F,Huang J L,Yang Y.Upper mantle structurebeneath the Chinese capital region from teleseismic finite-frequency tomography.Chinese J.Geophys.(in Chinese),2010,53(8):1806-1816.
[25]张学民,刁桂苓,赵英萍等.华北地区深部地幔剪切波速度结构研究.地球物理学报,2006,49(6):1709-1719.Zhang X M,Diao G L,Zhao Y P,et al.Study on mantleshear wave velocity structures in North China.Chinese J.Geophys.(in Chinese),2006,49(6):1709-1719.
[26]Ding Z F,Zhou X F,Wu Y,et al.Tomographic imaging ofP wave velocity structure beneath the region around Beijing.Earthq.Sci.,2009,22(4):403-408.
[27]张风雪,李永华,吴庆举等.FMTT方法研究华北及邻区上地幔P波速度结构.地球物理学报,2011,54(5):1233-1242.Zhang F X,Li Y H,Wu Q J,et al.The P wave velocitystructure of upper mantle beneath the North China andsurrounding regions from FMTT.Chinese J.Geophys.(inChinese),2011,54(5):1233-1242.
[28]Huang J L,Zhao D P.High-resolution mantle tomography ofChina and surrounding regions.J.Geophys.Res.,2006,111:B09305,doi:10.1029/2005JB004066.
[29]滕吉文,冯炽芬,李金森等.华北平原中部地区深部构造背景及邢台地震(一).地球物理学报,1974,17(4):255-272.Teng J W,Feng C F,Li J S,et al.Crustal structure of thecentral part of North China Plain and the Hsintai(邢台)earthquake(1).Chinese J.Geophys.(in Chinese),1974,17(4):255-272.
[30]滕吉文,王国正,刘道洪等.华北平原中部地区深部构造背景及邢台地震(二).地球物理学报,1975,18(3):196-207.Teng J W,Wang G Z,Liu D H,et al.Crustal structure ofthe central part of the North China Plain and the Hsingtai(邢台)earthquake(Ⅱ).Chinese J.Geophys.(in Chinese),1975,18(3):196-207.
[31]Wang C Y,Zhang X K,Lin Z Y,et al.Crustal structurebeneath the Xingtai earthquake area in North China and itstectonic implications.Tectonophysics,1997,274(4):307-319.
[32]Zhang Z J,Chen Q F,Bai Z M,et al.Crustal structure andextensional deformation of thinned lithosphere in NorthernChina.Tectonophysics,2011,508(1-4):62-72.
[33]何正勤,叶太兰,丁志峰.华北东北部的面波相速度层析成像研究.地球物理学报,2009,52(5):1233-1242.He Z Q,Yie T L,Ding Z F.Surface wave tomography forthe phase velocity in the northeastern part of North China.Chinese J.Geophys.(in Chinese),2009,52(5):1233-1242.
[34]于湘伟,陈运泰,张怀.京津唐地区地壳三维P波速度结构与地震活动性分析.地球物理学报,2010,53(8):1817-1828.Yu X W,Chen Y T,Zhang H.Three-dimensional crustal P-wave velocity structure and seismicity analysis in Beijing-Tianjin-Tangshan Region.Chinese J.Geophys.(inChinese),2010,53(8):1817-1828.
[35]唐有彩,冯永革,陈永顺等.山西断陷带地壳结构的接收函数研究.地球物理学报,2010,53(9):2102-2109.Tang Y C,Feng Y G,Chen T S,et al.Receiver functionanalysis at Shanxi Rift.Chinese J.Geophys.(in Chinese),2010,53(9):2102-2109.
[36]刘保金,胡平,孟勇奇等.北京地区地壳精细结构的深地震反射剖面探测研究.地球物理学报,2009,52(9):2264-2272.Liu B J,Hu P,Meng Y Q,et al.Research on fine crustalstructure using deep seismic reflection profile in Beijingregion.Chinese J.Geophys.(in Chinese),2009,52(9):2264-2272.
[37]王峻,刘启元,陈九辉等.根据接收函数反演得到的首都圈地壳上地幔三维S波速度结构.地球物理学报,2009,52(10):2472-2482.Wang J,Liu Q Y,Chen J H,et al.Three-dimensional S-wave velocity structure of the crust and upper mantle beneaththe Capital Circle Region from receiver function inversion.Chinese J.Geophys.(in Chinese),2009,52(10):2472-2482.
[38]潘佳铁,吴庆举,李永华等.华北地区瑞雷面波相速度层析成像.地球物理学报,2011,54(1):67-76.Pan J T,Wu Q J,Li Y H,et al.Rayleigh wave tomographyof the phase velocity in North China.Chinese J.Geophys.(in Chinese),2011,54(1):67-76.
[39]张永谦,滕吉文,王夫运等.阴山造山带及鄂尔多斯盆地北部地区上地壳的地震波属性结构及岩性推断.地球物理学报,2011,54(1):87-97.Zhang Y Q,Teng J W,Wang F Y,et al.Structure of theseismic wave property and lithology deduction of the uppercrust beneath the Yinshan orogenic belt and the northernOrdos block.Chinese J.Geophys.(in Chinese),2011,54(1):87-97.
[40]王鑫,詹艳,赵国泽等.鄂尔多斯盆地西缘构造带北段深部电性结构.地球物理学报,2010,53(3):595-604.Wang X,Zhan Y,Zhao G Z,et al.Deep electric structurebeneath the northern section of the western margin of theOrdos basin.Chinese J.Geophys.(in Chinese),2010,53(3):595-604.
[41]Fang L H,Wu J P,Ding Z F,et al.High resolutionRayleigh wave group velocity tomography in North Chinafrom ambient seismic noise.Geophys.J.Int.,2010,181(2):1171-1182.
[42]李传金,徐佩芬,孙勇军等.用远震接收函数研究山西地区地壳厚度变化:“晋中坡折带”及其地质意义探讨.地球物理学报,2010,53(5):1143-1148.Li C J,Xu P F,Sun Y J,et al.The Jinzhong transition beltand its geological significance by receiver function in Shanxiregion.Chinese J.Geophys.(in Chinese),2010,53(5):1143-1148.