引文
[1]朱守彪,张培震,石耀霖.华北盆地强震孕育的动力学机制研究.地球物理学报,2010,53(6):1409-1417.Zhu S B,Zhang P Z,Shi Y L.A study on the mechanisms ofstrong earthquake occurrence in the North China basin.Chinese J.Geophys.(in Chinese),2010,53(6):1409-1417.
[2]Gao S,Roberta R L,Yuan H L,et al.Recycling lowercontinental crust in the North China craton.Nature,2004,432(7019):892-897.
[3]邓晋福,莫宣学,赵海玲等.中国东部岩石圈根/去根作用与大陆“活化”──东亚型大陆动力学模式研究计划.现代地质,1994,8(3):349-356.Deng J F,Mo X X,Zhao H L,et al.Lithosphere root/de-rooting and activation of the east China continent.Geoscience(in Chinese),1994,8(3):349-356.
[4]Menzies A M,Fan W,Zhang M.Palaeozoic and Cenozoiclithoprobes and the loss of>120km of Archaean lithosphere,Sino-Korean craton,China.The Geological Society,1993,76(1):71-81.
[5]Zhu R X,Zheng T Y.Destruction geodynamics of the NorthChina Craton and its Paleoproterozoic plate tectonics.ChineseScience Bulletin,2009,54(19):3354-3366.
[6]毛桐恩,陈锦标,姚家榴.邢台、唐山震区震源层及其顶、底部介质条件的综合分析.地震学报,1996,18(1):89-96.Mao T E,Chen J B,Yao J L.Analysis of the upper andbottom boundary of Xingtai and Tangshan earthquake zone.Acta Seismologica Sinica(in Chinese),1996,18(1):89-96.
[7]刁桂苓,于利民,李钦祖等.唐山和澜沧地震序列震源区应力场的对比分析.地震学报,1995,17(3):305-311.Diao G L,Yu L M,Li Q Z,et al.Comparison of the stressfield between Tangshan and Lancang earthquake series.ActaSeismologica Sinica(in Chinese),1995,17(3):305-311.
[8]梅世蓉.邢台地震孕育发生模型及其前兆机理探讨.地震,1999,19(1):1-10.Mei S R.Model of preparation and generation of xingtaiearthquake and mechanism of its precursors.Earthquake(inChinese),1999,19(1):1-10.
[9]邵学钟,张家茹,章思亚等.邢台地震区深部构造背景的地震转换波探测和研究.地球物理学报,1993,36(5):610-620.Shao X Z,Zhang J R,Zhang S Y,et al.Study of deepstructures in xingtai earthquake area by method of convertedwaves of earthquakes.Chinese J.Geophys.(in Chinese),1993,36(5):610-620.
[10]曾融生,张少泉,周海南等.唐山地震区的地壳结构及大陆地震成因的探讨.地震学报,1985,7(2):126-140.Zeng R S,Zhang S Q,Zhou H N,et al.Crustal structure ofTangshan epicentral region and its relation to the seismogenicprocess of a continental earthquake.ActaS eismologica Sinica(inChinese),1985,7(2):126-140.
[11]邵学钟,张家茹,章思亚等.唐山大震区深部构造的初步研究.地球物理学报,1986,29(1):29-40.Shao X Z,Zhang J R,Zhang S Y,et al.Investigation of deepstructures in Tangshan earthquake area.Chinese J.Geophys.(in Chinese),1986,29(1):29-40.
[12]刘启元,王峻,陈九辉等.1976年唐山大地震的孕震环境:密集地震台阵观测得到的结果.地学前缘,2007,14(6):206-212.Liu Q Y,Wang J,Chen J H,et al.Seismogenic tectonicenvironment of 1976 great Tangshan earthquake:resultsgiven by dense seismic array observations.Earth ScienceFrontiers(in Chinese),2007,14(60):205-213.
[13]王峻,刘启元,陈九辉等.首都圈地区的地壳厚度及泊松比.地球物理学报,2008,52(1):58-65.Wang J,Liu Q Y,Chen J H,et al.The crustal thicknessand poisson′s ratio beneath the capital circle region.ChineseJ.Geophys.(in Chinese),2008,52(1):58-65.
[14]Shedlock K M,Baranowsk J,Xiao W W,et al.TheTangshan aftershock sequence.J.Geophys.Res.,1987,92(B3):2792-2803.
[15]藏绍先,杨军亮.我国华北等地区板内地震的深度分布及其物理背景.地震地质,1984,6(5):67-75.Zang S X,Yang J L.Distribution of focal depths forintraplate earthquakes in North China and its physicalexplanation.Seismology and Geology(in Chinese),1984,6(5):67-75.
[16]Nábělek J,Chen W P,Ye H.The Tangshan earthquakesequence and its implications for the evolution of the NorthChina basin.J.Geophys.Res.,1987,92:12615-12628.
[17]叶洪,张文郁.初论华北板内地震断层特征及其与地壳、上地幔动力学过程的关系.地震地质,1980,2(1):23-37.Ye H,Zhang W Y.The characteristics of intraplateearthquake faults in North China and their relationship to thedynamical processes in earth′s crust and uppermost mantle.Seismology and Geology(in Chinese),1980,2(1):23-37.
[18]陈运泰,林邦慧,林中洋等.根据地面形变的观测研究1966年邢台地震的震源过程.地球物理学报,1975,18(3):164-182.Chen Y T,Lin B H,Lin Z Y,et al.The focal mechanism ofthe 1966 Hsingta earthquake as inferred from the grounddeformation observations.Chinese J.Geophys.(in Chinese),1975,18(3):164-182.
[19]徐锡伟,于贵华,王峰等.1966年邢台地震群的发震构造模型——新生断层形成?先存活断层摩擦粘滑?中国地震,2000,16(4):364-378.Xu X W,Yu G H,Wang F,et al.Seismogenic model for the1966 Xingtai Earthquakes-nucleation of new-born fault orstrick-slip of pre-existing fault?Earthquake Research inChina(in Chinese),2000,16(4):364-378.
[20]陈祖安,白武明,林邦慧等.1966年以来华北地区一系列七级大震破裂过程的数值模拟.地球物理学报,2003,46(3):373-381.Chen Z A,Bai W M,Lin B H,et al.Numerical simulationfor rupture processes of a series of strong earthquakes(MS>7)inNorth China since 1966.Chinese J.Geophys.(in Chinese),2003,46(3):373-381.
[21]张之立,王成宝,方兴等.唐山地震破裂过程的雁行断裂模式及理论和试验的模拟.地震学报,1989,(3):291-301.Zhang Z L,Wang C B,Fang X,et al.An echelon fracturemodel for the Tangshan earthquake sequence as well assimulation in theory and experiment.Acta SeismologicaSinica(in Chinese),1989,(3):291-301.
[22]张宏志,刁桂苓,赵英萍等.邢台地区近年的震源机制.大地测量与地球动力学,2007,27(6):91-95.Zhang H Z,Diao G L,Zhao Y P,et al.Recent focalmechanism in Xingtai region.Journal of Geodesy andGeodynamics(in Chinee),2007,27(6):91-95.
[23]潘波,许建东,刘启方.1679年三河-平谷8级地震近断层强地震动的有限元模拟.地震地质,2009,31(1):69-83.Pan B,Xu J D,Liu Q F.Simulations of the near-fault strongground motion of the 1679Sanhe-Pinggu M8.0earthquake.Seismology and Geology(in Chinese),2009,31(1):69-83.
[24]冉勇康,邓起东,杨晓平等.1679年三河—平谷8级地震发震断层的古地震及其重复间隔.地震地质,1997,19(3):194-201.Ruan Y K,Deng Q D,Yang X P,et al.Paleo-earthquakesand recurrence interval on the seismogenic fault of 1697Sanhe-Pinggu M8.0earthquake,Hebei and Beijing.Seismologyand Geology(in Chinese),1997,19(3):194-201.
[25]魏光兴,季同仁,李秉峰.渤海地震序列及其特征.地震地质,1984,6(1):22-29.Wei G X,Ji T R,Li B F.Characteristics of magnitude 7.4earthquake equence in the Bohai area.Seismology andGeology(in Chinese),1984,6(1):22-29.
[26]束沛镒,李幼铭,铁安等.利用远震P波波形反演渤海地震的震源参数.地球物理学报,1983,26(1):31-38.Shu P Y,Li Y M,Tie A,et al.An inversion of the focusparameters of Bohai earthquake from the teleseismic P waveshape.Chinese J.Geophys.(in Chinese),1983,26(1):31-38.
[27]宋惠珍,高维安,孙君秀等.唐山地震震源应力场的数值模拟研究——三维有限单元法在计算震源应力场中的应用.西北地震学报,1982,(3):32-38.Song H Z,Gao W A,Sun J X,et al.Numerical modellingthe stress field in Tangshan earthquake—application of 3Dmodelling stress field by FEM.Northwest China SeismologicalJournal(in Chinese),1982,(3):32-38.
[28]郑治真,刘元壮,胡祚春.唐山地震孕育过程的数学模拟——(二)地震孕育过程的数学模拟.地震研究,1984,(3):51-58.Zhen Z Z,Liu Y Z,Hu Z C.The numerical simulation ofpreparatory process of Tangshan earthquake.(2)A numericalsimulation of preparatory process of earthquake.Journal ofSeismological Research(in Chinese),1984,(3):51-58.
[29]张东宁,曾融生.冀中坳陷滑脱构造动力的数值模拟.地震学报,1995,17(4):414-421.Zhang D N,Zeng R S.Numerical modelling the detachmentof Jizhong depression area.Acta Seismologica Sinica(inChinese),1995,17(4):414-421.
[30]王继存,续春荣.唐山地震断层破坏及其力学过程的数值模拟.地震地质,1989,11(4):71-76.Wang J C,Xu C R.Fault failure by Tangshan earthquakeand numerical analogue of its mechanical process.Seismologyand Geology(in Chinese),1989,11(4):71-76.
[31]梅世蓉,梁北援.唐山地震孕震过程的数值模拟.中国地震,1989,(3):42-47.Mei S R,Liang B Y.A mathematical simulation forseismogenetic process of the Tangshan earthquake.EarthquakeResearch in China(in Chinese),1989,(3):42-47.
[32]冯德益,刘喜兰,舒立德等.唐山7.8级强震孕育条件及前兆场时空演化的三维数值模拟计算与分析.华北地震科学,1996,(4):43-52.Feng D Y,Liu X L,Shu L D,et al.Three-dimensionalnumerical simulation and analysis of seismogenic conditionand temporo-spatial evolution of precursor field of TangshanM=7.8great earthquake.North China Earthquake Sciences(in Chinese),1996,(4):43-52.
[33]尹京苑,梅世蓉.邢台强震区的深部构造对强震孕育影响的三维数值模拟.地球物理学报,1999,42(增刊):131-140.Yin J Y,Mei S Y.3-D simulation for the effect of deepstructures to the preparation of strong earthquake in Xingtaiarea.Chinese J.Geophys.(in Chinese),1999,42(Suppl.):131-140.
[34]孙武城,李松林,张晓普.华北大陆地壳-上地幔波浪断裂型构造的光弹模拟实验.华北地震科学,1983,1(1):21-27.Sun W C,Li S L,Zhang X P.Photoelastic experiment on thefailure structure of the fluctuating Moho surface in NorthChina continent.North China Earthquake Sciences(inChinese),1983,1(1):21-27.
[35]肖兰喜,朱元清,张少泉等.邢台震区深部构造与强震孕育关系的探讨.地震学报,1999,21(6):597-607.Xiao L X,Zhu Y Q,Zhang S Q,et al.The relationshipbetween the deep-level structure in crust and brewing ofstrong earthquakes in Xingtai area.Acta Seismologica Sinica(in Chinese),1999,21(6):597-607.
[36]宋治平,尹祥础,梅世蓉.地震孕育体源流变模型(二)——应变场及其应用.地震学报,2004,26(2):121-131.Song Z P,Yin X C,Mei S R.3-D rheologic model ofearthquake preparation(2).Strain field and its applications.Acta Seismologica Sinica(in Chinese),2004,26(2):121-131.
[37]金安蜀,刘福田,孙永智.北京地区地壳和上地幔的三维P波速度结构.地球物理学报,1980,23(2):172-182.Jin A S,Liu F T,Sun Y Z.Three-dimensional P velocitystructure of the crust and upper mantle under Beijing region.Chinese J.Geophys.(in Chinese),1980,23(2):172-182.
[38]刘福田,曲克信,吴华等.华北地区的地震层面成象.地球物理学报,1986,29(5):442-449.Liu F T,Qu K X,Wu H,et al.Seismic tomography ofNorth China region.Chinese J.Geophys.(in Chinese),1986,29(5):442-449.
[39]林真明,邵学钟,陈学波.1966年邢台地震区地震测深资料再解释.华北地震科学,1990,(3):34-37.Lin Z M,Shao X Z,Chen X B.Reanalyzing for the seismicsounding data in Xingtai seismic area in 1966.North ChinaEarthquake Sciences(in Chinese),1990,(3):34-37.
[40]孙若昧,刘福田.京津唐地区地壳结构与强震的发生——1.P波速度结构.地球物理学报,1995,38(5):599-607.Sun R M,Liu F T.Crust structure and strong earthquake inBeijing,Tianjing,Tangshan area:I.P wave velocitystructure.Chinese J.Geophys.(in Chinese),1995,38(5):599-607.
[41]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-Tianjing-Tangshan area.ActaSeismologica Sinica(in Chinese),2003,25(1):1-14.
[42]梅世蓉,梁北援.唐山地震孕震过程的数值模拟.中国地震,1989,(3):42-47.Mei S R,Liang B Y.A mathematical simulation forseismogenetic process of the Tangshan earthquake.EarthquakeResearch in China(in Chinese),1989,(3):42-47.
[43]张家茹,邵学钟,章思亚等.邢台强震的深部三维构造背景和孕震条件.地震地质,1994,(4):21-27.Zhang J R,Shao X Z,Zhang S Y,et al.Background of 3-Ddeep structure and dynamic conditions for occurrence ofstrong Xingtai earthquake.Seismology and Geology(inChinese),1994,(4):21-27.
[44]赖晓玲,张先康,郑需要.利用三维弯曲界面的反演方法重建唐山震区莫霍界面三维构造形态.地震学报,1997,19(5):506-516.Lai X L,Zhang X K,Zheng X Y.Rebuilding the Mohosurface of Tangshan earthquake zone using bending surfaceinversion.Acta Seismologica Sinica(in Chinese),1997,19(5):506-516.
[45]An M J,Feng M,Zhao Y.Destruction of lithosphere withinthe north China craton inferred from surface wave tomography.Geochemistry Geophysics Geosystems,2009,10:Q08016.
[46]Huang J L,Zhao D P,Zheng S H.Lithospheric structureand its relationship to seismic and volcanic activity insouthwest China.J.Geophys.Res.,2002,111:2255.
[47]臧绍先,李昶,宁杰远等.华北岩石圈三维流变结构的一种初步模型.中国科学(D),2002,32(7):588-597.Zang S X,Li C,Ning J Y,et al.3Drheology model of thelithosphere of North China basin.Science China(D)(inChinese),2002,32(7):588-597.
[48]安美建,石耀霖.中国大陆地壳和上地幔三维温度场.中国科学(D),2007,37(6):736-745.An M J,Shi Y L.3Dtemperature of crust and lithospheremantle in Chinese continent.Science China(D)(in Chinese),2007,37(6):736-745.
[49]石耀霖,曹建玲.中国大陆岩石圈等效粘滞系数的计算和讨论.地学前缘,2008,15(3):83-95.Shi Y L,Cao J L.Effective viscosity of China continentallithosphere.Earth Sciences Frontier(in Chinese),2008,15(3):83-95.
[50]Li Z H,Gerya T V.Polyphase formation and exhumation ofhigh-to ultrahigh-pressure rocks in continental subductionzone:Numerical modeling and application to the Suluultrahigh-pressure terrane in eastern China.J.Geophys.Res.,2009,114:B09406.
[51]Li Z H,Gerya T V,Burg J P.Influence of tectonicoverpressure on P-T paths of HP-UHP rocks in continentalcollision zones:Thermomechanical modeling.Journal ofMetamorphic Geology,2010,28(3):227-247.
[52]Li Z H,Xu Z Q,Gerya T V.Flat versus steep subduction:contrasting modes for the formation and exhumation of high-toultrahigh-pressure rocks in continental collision zones.Earth andPlanetary Science Letters,2011,301(1-2):65-77.
[53]李钦祖.华北地壳应力场的基本特征.地球物理学报,1980,23(4):376-388.Li Q Z.General features of the stress field in the crust ofNorth China.Chinese J.Geophys.(in Chinese),1980,23(4):376-388.
[54]李延兴,徐杰,陈聚忠等.邢台、渤海、海城和唐山大地震震中区现今应变场的基本特征.华北地震科学,2006,24(2):36-39.Li Y X,Xu J,Chen J Z,et al.Basic characteristics ofcurrent strain field in the epicentral area of Xingtai,Bohai,Haicheng and Tangshan strong earthquake.North ChinaEarthquake Sciences(in Chinese),2006,24(2):36-39.
[55]白武明,林邦慧,陈祖安.1976年唐山大震发生对华北地区各地块运动与变形影响的数值模拟研究.中国科学,2003,33(增刊):99-107.Bai W M,Lin B H,Chen Z A.Numerical modelling theblock motion and deformation induced by Tangshanearthquake.Science in China(D)(in Chinese),2003,33(Suppl.):99-107.
[56]柳畅,朱伯靖,石耀霖.粘弹性数值模拟龙门山断裂带应力积累及大震复发周期.地质学报,2012,86(1):157-169.Liu C,Zhu B J,Shi Y L.Stress accumulation of theLongmenshan fault and recurrence interval of Wenchuanearthquake based on viscoelasticity simulation.Acta GeologicaSinica(in Chinese),2012,86(1):157-169.
[57]李轶群,王健.唐山余震区中小地震震源机制解分区特征的初步研究.中国地震,2008,24(2):150-157.Li Y Q,Wang J.The preliminary study on focal mechanismof small and moderate earthquakes in divided zones aroundTangshan.Earthquake Research in China(in Chinese),2008,24(2):150-157.
[58]兰从欣,邢成起,苗春兰等.近年首都圈地区中小地震震源机制解及其特征分析.华北地震科学,2005,24(3):22-25.Lan C X,Xing C Q,Miao C L,et al.The focal mechanismsolutions and their characteristics for moderate and smallearthquakes in Capital Area in recent years.North ChinaEarthquake Sciences(in Chinese),2005,24(3):22-25.
[59]韦生吉,倪四道,崇加军等.2003年8月16日赤峰地震:一个可能发生在下地壳的地震?地球物理学报,2009,52(1):111-119.Wei S J,Ni S D,Chong J J,et al.The 16 August 2003Chifeng earthquake:Is it a lower crust earthquake?ChineseJ.Geophys.(in Chinese),2009,52(1):111-119.
[60]赖晓玲,李松林,孙译.渤海及邻区3次7级以上地震的深部构造背景.大地测量与地球动力学,2007,27(1):31-33,54.Lai X L,Li S L,Sun Y.Deep tectonic background of threeMS>7.0strong earthquakes in Bohai and its adjacent region.Journal of Geodesy and Geodynamics(in Chinese),2007,27(1):31-33,54.
[61]徐菊生,袁金荣,高士钧.利用GPS观测结果研究华北地区现今构造应力场.地壳形变与地震,1999,19(2):81-89.Xu J S,Yuan J R,Gao S J.Research on the precent tectonicstress field in North China with GPS observations.CrustalDeformation and Earthquake(in Chinese),1999,19(2):81-89.
[62]袁金荣,徐菊生,高士钧.利用GPS观测资料反演华北地区现今构造应力场.地球学报,1999,20(3):232-238.Yuan J R,Xu J S,Gao S J.Back analysis of present tectonicstress field in North China region using GPS data.ActaGeoscientia Sinica(in Chinese),1999,20(3):232-238.
[63]陈连旺,陆远忠,张杰等.华北地区三维构造应力场.地震学报,1999,21(2):140-149.Chen L W,Lu Y Z,Zhang J,et al.There dimensionaltectonic stress field in North China.Acta Seismologica Sinica(in Chinese),1999,21(2):140-149.
[64]Harris R A.Introduction to special section:Stress triggers,stress shadows,and implications for seismic hazard.J.Geophys.Res.,1998,103(B10):24347-24358.
[65]石耀霖.关于应力触发和应力影概念在地震预报中应用的一些思考.地震,2001,21(3):1-7.Shi Y L.Stress triggers and stress shadows:How to applythese concepts to earthquake prediction.Earthquake,2001,21(3):1-7.
[66]曾融生,朱露培,何正勤等.华北盆地强震的震源模型兼论强震和盆地的成因.地球物理学报,1991,34(3):288-301.Zeng R S,Zhu L P,He Z Q,et al.Model of the earthquakesource of North China basin strong earthquake and discussionthe mechanism of extensional basin.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1991,34(3):288-301.
[67]熊熊,许厚泽.地幔对流诱发的莫霍面起伏与下地壳塑性流动.测绘学报,2000,29(增刊):21-25.Xiong X,Xu H Z.Undulation of Moho and ductile flow oflower crust induced by mantle flow.Acta Geodaetica etCartographica Sinica(in Chinese),2000,29(Suppl.):21-25.
[68]石耀霖,朱守彪.中国大陆震源机制深度变化反映的地壳、地幔流变特征.地球物理学报,2003,46(3):359-365.Shi Y L,Zhu S B.Contrast of rheology in the crust andmantle near Moho revealed by depth variation of earthquakemechanism in continental China.Chinese J.Geophys.(inChinese),2003,46(3):359-365.
[69]McKenzie D P,Nimmo F,Jackson A J,et al.Characteristicsand consequences of flow in the lower crust.J.Geophys.Res.,2000,105(B5):11029-11046.
[70]Gans P B.An open-system two layer crustal stretching modelfor the eastern Great basin.Tectonics,1987,6(1):1-12.
[71]Kusznir H N,Matehews H D.Deep seismic reflections andthe deformational mechanics of the continental lithosphere.J.Petrol.,1988,Special Lithosphere Issue:63-87.
[72]汪素云,陈培善.中国及邻区现代构造应力场的数值模拟.地球物理学报,1980,23(1):35-45.Wang S Y,Chen P S.A numerical simulation of the presenttectonic stress field of china and its vicinity.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1980,23(1):35-45.