基于背景噪声成像方法研究郯庐断裂带中南段及邻区地壳速度结构与变形特征
|
摘要
郯庐断裂带是贯穿我国东部北北东走向的一条深大断裂,其中南段及其邻区(115°E—121°E,29.5°N—35°N)穿过了大别造山带、苏鲁造山带、长江中下游成矿带及合肥盆地.为了研究该区域地壳速度结构及变形特征,我们使用安徽省和江苏省及其周边地区105个台站(固定台站98个,流动台站7个)的垂向连续波形数据,时间范围从2014年5月到2015年7月,共计14个月.利用背景噪声互相关方法,从垂直分量互相关函数中最终提取了2590条瑞利面波相速度频散曲线,反演得到周期范围为5～30s的瑞利波方位各向异性相速度分布图,再反演每个网格点瑞利面波相速度频散得到一维层状横波速度模型,然后拼合起来组成三维横波速度模型.根据本文反演结果并综合已有资料,我们得出如下结论:(1)在北大别、蚌埠隆起、长江中下游成矿带、合肥盆地北部大桥凹陷区域存在中地壳横波高速体,可能与岩石圈和下地壳拆沉以及中生代中国东部大范围岩浆活动有直接关系,更深层原因可能与古太平洋俯冲相关;(2)苏鲁造山带南缘,垂直于嘉山响水断裂,从南向北中上地壳低速体深度变浅,这个低速体可能是高压/超高压变质岩与扬子板块接触处的破碎带,是扬子板块与华北板块接触的边界;(3)郯庐断裂合肥—嘉山段两侧以及大别造山带东缘短周期瑞利面波相速度快轴方向与郯庐断裂带走向基本一致,可能是三叠纪碰撞期与白垩纪时期的大规模左旋走滑活动的结果;(4)合肥盆地南部15～20s周期的瑞利波相速度快轴方向为北西-南东向,反应该区域中下地壳快波方向为北西-南东向,推测是大别造山带折返的痕迹;(5)郯庐断裂带的结构和地震活动性存在明显的分段性,嘉山—郯城段郯庐断裂带现今地震活动性弱,但发生过较强的古地震,推断现今郯庐断裂带宿迁段可能处于闭锁状态,从长远来看要注意该地区发生大震的可能.
Tanlu fault is a deep penetrating fault with an NNE strike in eastern China.Its central-southern segment and the adjacent area traverse the Dabie orogenic belt,the Sulu orogenic belt,the Middle-Lower Yangtze metallogenic belt,and the Heifei Basin.In order to study the crustal velocity structure and deformation characteristics in this region,we used continuous waveform data from May 2014 to July 2015,a total of 14 months,of 105 stations(98 permanent stations and 7 temporary stations)in Anhui and Jiangsu Provinces and its surrounding area.Using the ambient noise cross-correlation method,we finally extracted 2590 surface Rayleigh wave phase velocity dispersion curves from the vertical component cross-correlation function,and then obtained an azimuthally anisotropic Rayleigh wave phase velocity maps in the period band 5～30 s.Then we inverted the Rayleigh wave phase velocity dispersion at each grid point for a onedimensional layered shear velocity model,which was then combined to form a three-dimensional shear velocity model.Based on the inversion results and the existed data,we draw the conclusions as follows.(1)The northern Dabie orogenic belt,Bengbu uplift,Middle-Lower Yangtze metallogenic belt,and Daqiao-Dingyuan depression in the northern Hefei Basin exhibit higher shear velocity anomalies in the middle crust,which may be directly related to the lithosphere and lower crust delamination and Mesozoic volcanic magmatism in eastern China,and the deeper causes may be related to the Paleo-Pacific subduction.(2)The low velocity body shallows from south to north in the upper-middle crust of the southern margin of the Sulu orogenic belt,which is perpendicular to the Jiashui-Xiangshui fault.The low velocity body may be the fracture zone where the ultra-high/high pressure metamorphic rocks come into contact with the Yangtze plate.It is a contact boundary between the Yangtze plate and the North China plate.(3)The fast-axis direction of the short period Rayleigh wave phase velocity on both sides of the Hefei-Jiashan section of the Tanlu fault and the eastern boundary of the Dabie orogenic belt is basically consistent with strike of the Tanlu fault,which may be the result of the large-scale sinistral strike-slip activity of the Tanlu fault during the Triassic collision period and the Cretaceous;(4)The fast-axis direction of Rayleigh wave in the period band 15～20 sis northwest-southeast in the south of the Hefei Basin,indicating a northwest-southeast fast wave direction in the middle and lower crust in this area,presumably reflecting the trace of the exhumation of the Dabie orogenic belt.(5)The structure and seismicity of the Tanlu fault zone are clearly segmented.The seismicity of the Tanlu fault from Jiashan to Tancheng is weak at present,but strong paleo-earthquakes occurred.It is inferred that the Suqian section of the Tanlu fault may be in a locking state.In the long run,attention should be paid to the possibility of large earthquakes occurring in this area.
Tanlu fault is a deep penetrating fault with an NNE strike in eastern China.Its central-southern segment and the adjacent area traverse the Dabie orogenic belt,the Sulu orogenic belt,the Middle-Lower Yangtze metallogenic belt,and the Heifei Basin.In order to study the crustal velocity structure and deformation characteristics in this region,we used continuous waveform data from May 2014 to July 2015,a total of 14 months,of 105 stations(98 permanent stations and 7 temporary stations)in Anhui and Jiangsu Provinces and its surrounding area.Using the ambient noise cross-correlation method,we finally extracted 2590 surface Rayleigh wave phase velocity dispersion curves from the vertical component cross-correlation function,and then obtained an azimuthally anisotropic Rayleigh wave phase velocity maps in the period band 5～30 s.Then we inverted the Rayleigh wave phase velocity dispersion at each grid point for a onedimensional layered shear velocity model,which was then combined to form a three-dimensional shear velocity model.Based on the inversion results and the existed data,we draw the conclusions as follows.(1)The northern Dabie orogenic belt,Bengbu uplift,Middle-Lower Yangtze metallogenic belt,and Daqiao-Dingyuan depression in the northern Hefei Basin exhibit higher shear velocity anomalies in the middle crust,which may be directly related to the lithosphere and lower crust delamination and Mesozoic volcanic magmatism in eastern China,and the deeper causes may be related to the Paleo-Pacific subduction.(2)The low velocity body shallows from south to north in the upper-middle crust of the southern margin of the Sulu orogenic belt,which is perpendicular to the Jiashui-Xiangshui fault.The low velocity body may be the fracture zone where the ultra-high/high pressure metamorphic rocks come into contact with the Yangtze plate.It is a contact boundary between the Yangtze plate and the North China plate.(3)The fast-axis direction of the short period Rayleigh wave phase velocity on both sides of the Hefei-Jiashan section of the Tanlu fault and the eastern boundary of the Dabie orogenic belt is basically consistent with strike of the Tanlu fault,which may be the result of the large-scale sinistral strike-slip activity of the Tanlu fault during the Triassic collision period and the Cretaceous;(4)The fast-axis direction of Rayleigh wave in the period band 15～20 sis northwest-southeast in the south of the Hefei Basin,indicating a northwest-southeast fast wave direction in the middle and lower crust in this area,presumably reflecting the trace of the exhumation of the Dabie orogenic belt.(5)The structure and seismicity of the Tanlu fault zone are clearly segmented.The seismicity of the Tanlu fault from Jiashan to Tancheng is weak at present,but strong paleo-earthquakes occurred.It is inferred that the Suqian section of the Tanlu fault may be in a locking state.In the long run,attention should be paid to the possibility of large earthquakes occurring in this area.
引文
Bensen G D,Ritzwoller M H,Barmin M P,et al.2007.Processing seismic ambient noise data to obtain reliable broad-band surface wave dispersion measurements.Geophysical Journal International,169(3):1239-1260.
Bensen G D,Ritzwoller M H,Shapiro N M.2008.Broadband ambient noise surface wave tomography across the United States.Journal of Geophysical Research:Solid Earth,113(B5):B05306,doi:10.1029/2007JB005248.
Chang L J.2014.Constraining the dynamic characteristics of lithosphere and asthenosphere in Mainland China and its adjacent regions using GPS,Quaternary fault slip rates and shear wave splitting data[Ph.D.thesis](in Chinese).Beijing:Institute of Geophysics,China Earthquake Administration.
Cong B L,Wang Q C,Zhang H Z,et al.1996.Petrogenesis of Cenozoic volcanic rocks in Hefei basin,China.Acta Petrologica Sinica(in Chinese),12(3):370-381.
Deng Y F,Fan W M,Zhang Z J,et al.2013.Geophysical evidence on segmentation of the Tancheng-Lujiang fault and its implications on the lithosphere evolution in East China.Journal of Asian Earth Sciences,2013,78:263-276.
Dong S W,Wu X Z,Gao R,et al.1998.On the crust velocity levels and dynamics of the Dabieshan orogenic belt.Acta Geophysica Sinica(in Chinese),41(3):349-361.
Hacker B R,Ratschbacher L,Webb L,et al.1998.U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling-Dabie Orogen,China.Earth and Planetary Science Letters,161(1-4):215-230.
Hacker B R,Ratschbacher L,Liou J G.2004.Subduction,collision and exhumation in the ultrahigh-pressure Qinling-Dabie orogen.Geological Society,London,Special Publications,2004,226(1):157-175.
He R Z,Shang X F,Yu C Q,et al.2014.A unified map of Moho depth and VP/VSratio of continental China by receiver function analysis.Geophysical Journal International,199(3):1910-1918.
Herrmann R B,Ammon C J.2002.Surface Waves,Receiver Functions and Crustal Structure,Computer Programs in Seismology,version3.30.Saint Louis:Saint Louis University.
Huang J L,Zhao D P.2006.High-resolution mantle tomography of China and surrounding regions.Journal of Geophysical Research:Solid Earth,111(B9):B09305,doi:10.1029/2005JB004066.
Huang R,Xu Y X,Zhu L P,et al.2015.Detailed Moho geometry beneath southeastern China and its implications on thinning of continental crust.Journal of Asian Earth Sciences,112:42-48.
Huang Y,Li Q H,Zhang Y S,et al.2011.Crustal velocity structure beneath the Shandong-Jiangsu-Anhui segment of the TanchengLujiang Fault Zone and adjacent areas.Chinese Journal of Geophysics(in Chinese),54(10):2549-2559,doi:10.3969/j.issn.0001-5733.2011.10.012.
Huang Z X,Su W,Peng Y J,et al.2003.Rayleigh wave tomography of China and adjacent regions.Journal of Geophysical Research:Solid Earth,108(B2):2073,doi:10.1029/2001JB001696.
Huang Z X,Xu Y,Hao T Y,et al.2009.Surface wave tomography of lithospheric structure in the seas of east China.Chinese Journal of Geophysics(in Chinese),52(3):653-662.
Jiang G M,Zhang G B,Lv Q T,et al.2013.3-D velocity model beneath the Middle-Lower Yangtze River and its implication to the deep geodynamics.Tectonophysics,606:36-47.
Jiang G M,Zhang G B,Lu Q T,et al.2014.Deep geodynamics of mineralization beneath the Middle-Lower Reaches of Yangtze River:Evidence from teleseismic tomography.Acta Petrologica Sinica(in Chinese),30(4):907-917.
Jin K,Xu W L,Wang Q H,et al.2003.Formation time and sources of the Huaiguang“Migmatitic Granodiorite”in Bengbu,Anhui Province:Evidence from SHRIMP zircon U-Pb geochronology.Acta Geoscientia Sinica(in Chinese),24(4):331-335.
LüJ,Xie Z J,Zheng Y,et al.2016.Rayleigh wave phase velocities of South China block and its adjacent areas.Science in China Earth Sciences,59(11):2165-2178.
LüQ T,Dong S W,Shi D N,et al.2014.Lithosphere architecture and geodynamic model of middle and lower reaches of Yangtze metallogenic belt:A review from SinoProbe.Acta Petrologica Sinica(in Chinese),30(4):889-906.
Leary P C,Crampin S,McEvilly T V.1990.Seismic fracture anisotropy in the Earth′s crust:An overview.Journal of Geophysical Research:Solid Earth,95(B7):11105-11114.
Li S Q,Chen F K,Siebel W,et al.2012.Late Mesozoic tectonic evolution of the Songliao basin,NE China:Evidence from detrital zircon ages and Sr-Nd isotopes.Gondwana Research,22(3-4):943-955.
Li S Z,Kusky T M,Zhao G C,et al.2010.Two-stage Triassic exhumation of HP-UHP terranes in the western Dabie orogen of China:Constraints from structural geology.Tectonophysics,490(3-4):267-293.
Lin W,Michel F,Wang Q C,et al.2005.Tectonic evolution of the Dabieshan orogen:In the view from polyphase deformation of the Beihuaiyang metamorphic zone.Science in China Series D:Earth Sciences,48(7):886-899.
Liu C M,Yao H J.2017.Surface wave tomography with spatially varying smoothing based on continuous model regionalization.Pure and Applied Geophysics,174(3):937-953.
Liu F T,Xu P F,Liu J S,et al.2003.The crustal velocity structure of the continental deep subduction belt:Study on the eastern Dabie orogen by seismic wide-angle reflection/refraction.Chinese Journal of Geophysics(in Chinese),46(3):366-372.
Liu S A,Li S G,Guo S S,et al.2012.The Cretaceous adakiticbasaltic-granitic magma sequence on south-eastern margin of the North China Craton:Implications for lithospheric thinning mechanism.Lithos,134-135:163-178.
Liu X Q,Yan J,Wang A G,et al.2016.Geochronological study on Mesozoic magmatic rocks in Yuexi area,Dabie Orogen.Geological Review(in Chinese),62(4):897-914.
Luo Y H,Xu Y X,Yang Y J.2012.Crustal structure beneath the Dabie orogenic belt from ambient noise tomography.Earth and Planetary Science Letters,313-314:12-22.
Luo Y H,Xu Y X,Yang Y J.2013.Crustal radial anisotropy beneath the Dabie orogenic belt from ambient noise tomography.Geophysical Journal International,195(2):1149-1164.
Montagner J P,Nataf H C.1986.A simple method for inverting the azimuthal anisotropy of surface waves.Journal of Geophysical Research:Solid Earth,91(B1):511-520.
Nafe J E,Drake C L.1957.Variation with depth in shallow and deep water marine sediments of porosity,density and the velocities of compressional and shear waves.Geophysics,22(3):523-713.
Ni H Y,Liu Z M,He K.2013.Study on focal mechanisms of moderatesmall earthquakes and characteristics of recent tectonic stress field in the Anhui sector of Tanlu fault zone.China Earthquake Engineering Journal(in Chinese),35(3):677-683.
Ouyang L B,Li H Y,Lv Q T,et al.2014.Crustal and uppermost mantle velocity structure and its relationship with the formation of ore districts in the Middle-Lower Yangtze River region.Earth and Planetary Science Letters,408:378-389.
Ouyang L B,Li H Y,LüQ T,et al.2015.Crustal shear wave velocity structure and radial anisotropy beneath the MiddleLower Yangtze River metallogenic belt and surrounding areas from seismic ambient noise tomography.Chinese Journal of Geophysics(in Chinese),58(12):4388-4402,doi:10.6038/cjg20151205.
Qiu R L,Xu X,Huang D Z.1999.The isotopic age of the Jingshan intrusive in the Bengbu region of the southeastern edge of the north china block and its geological implications.Geology of Anhui(in Chinese),9(3):161-164.
Shen W S,Ritzwoller M H,Kang D,et al.2016.A seismic reference model for the crust and uppermost mantle beneath China from surface wave dispersion.Geophysical Journal International,206(2):954-979.
Shi D N,LüQ T,Xu W Y,et al.2013.Crustal structure beneath the middle-lower Yangtze metallogenic belt in East China:Constraints from passive source seismic experiment on the Mesozoic intra-continental mineralization.Tectonophysics,606:48-59.
Tarantola A,Valette B.1982.Generalized nonlinear inverse problems solved using the least squares criterion.Review of Geophysics,20(2):219-232.
Wang C Y,Zhang X K,Ding Z F,et al.1997.Finite-difference tomography of upper crustal structure in Dabieshan orogenic belt.Acta Geophysica Sinica(in Chinese),40(4):495-502.
Wang Q,Zhao Z H,Xiong X L,et al.2001.Melting of the underplated basaltic lower crust:Evidence from the Shaxi adakitic sodic quartz diorite-porphyrites,Anhui Province,China.Geochimica(in Chinese),30(4):353-362.
Wang X F,Li Z J,Chen B L,et al.2005.On the Tan-Lu Fault Zone(in Chinese).Beijing:Geological Publishing House,12-13.
Wang Y J,Fan W M,Peng T P,et al.2005.Nature of the Mesozoic lithospheric mantle and tectonic decoupling beneath the Dabie Orogen,Central China:Evidence from 40 Ar/39 Ar geochronology,elemental and Sr-Nd-Pb isotopic compositions of early Cretaceous mafic igneous rocks.Chemical Geology,220(3-4):165-189.
Wei C J,Zhang L F,Wang S G.2001.Mesozoic high-K granitic rocks from the eastern Dabie Mountains,Central China and their geological implications.Science in China Series D:Earth Sciences,44(6):525-534.
Weiss T,Siegesmund S,Rabbel W,et al.1999.Seismic velocities and anisotropy of the lower continental crust:A review.Pure and Applied Geophysics,156(1-2):97-122.
Wu P P,Ding Z F,Ma X J,et al.2015.Rayleigh wave group velocity tomography beneath Dabie-Sulu and its adjacent areas from ambient seismic noise.Acta Seismologica Sinica(in Chinese),37(2):218-229.
Xie Z,Zheng Y F,Zhao Z F,et al.2006.Mineral isotope evidence for the contemporaneous process of Mesozoic granite emplacement and gneiss metamorphism in the Dabie orogen.Chemical Geology,231(3):214-235.
Xiong Z,LI Q H,Zhang Y S,et al.2016.Segmentation of crustal velocity structure beneath the Shandong-Jiangsu-Anhui segment of the Tanlu fault zone and adjacent areas and its geological implications.Chinese Journal of Geophysics(in Chinese),59(7):2433-2443,doi:10.6038/cjg20160710.
Xu J F,Shinjo R,Defant M J,et al.2002.Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China:Partial melting of delaminated lower continental crust?.Geology,30(12):1111-1114.
Xu J W,Cui K R,Zhu G,et al.1984.Some progress of displacement research of the Tan-Lu fault system,eastern China.Journal of Hefei Polytechnic University(in Chinese),(2):28-37.
Xu P F,Sun R M,Liu Fu T,et al.2000.Seismic tomography showing subduction and slab breakoff of the Yangtze block beneath the Dabie-Sulu orogenic belt.Chinese Science Bulletin,44(1):70-74.
Xu P F,Liu F T,Wang Q C,et al.2000.Seismic tomography beneath the Dabie-Sulu collision orogen 3-D velocity structures of lithosphere.Chinese Journal of Geophysics(in Chinese),43(3):377-385.
Xu T,Zhang Z J,Tian X B,et al.2014.Crustal structure beneath the Middle-Lower Yangtze metallogenic belt and its surrounding areas:Constraints from active source seismic experiment along the Lixin to Yixing profile in East China.Acta Petrologica Sinica(in Chinese),30(4):918-930.
Xu W L,Wang Q H,Yang D B,et al.2005.SHRIMP zircon U-Pb dating in Jingshan“migmatitic granite”,Bengbu and its geological significance.Science in China Series D:Earth Sciences,48(2):185-191.
Xu W L,Yang D B,Pei F P,et al.2006.Age of the Wuhe complex in the Bengbu uplift:Evidence from LA-ICP-MS zircon U-Pb dating.Geology in China(in Chinese),33(1):132-137.
Yang D B,Xu W L,Pei F P,et al.2005.Formation time and magma source of granites in Bengbu uplift:Evidence from LA-ICPMS zircon U-Pb dating and tracing.Geochimica(in Chinese),34(5):443-454.
Yang D B,Xu W L,Wang Q H,et al.2007.Petrogenesis of the Mesozoic granite in Bengbu uplift:Constraints from zircon Hf isotope.Acta Petrologica Sinica(in Chinese),23(2):381-392.
Yang W C,Hu Z Y,Cheng Z Y,et al.1999.Long profile of geophysical investigation from Tanchen to Lianshui,East-Central China.Chinese Journal of Geophysics(in Chinese),42(2):206-217.
Yang W C.2002.Geophysical profiling across the Sulu ultra-highpressure metamorphic belt,eastern China.Tectonophysics,354(3-4):277-288.
Yang Y,Wang W,Wang J F.2017.Characteristics of regional stress field and latest crustal deformation in middle-southern segment of Tan-Lu fault zone.China Earthquake Engineering Journal(in Chinese),39(S1):14-19.
Yang Y Y,Zhao P,Zheng H G,et al.2017.Evidence of holocene activity discovered in anhui ziyangshan segment of tanlu fault zone.Seismology and Geology(in Chinese),39(4):644-655.
Yao D Q,Yang Y Y,Zhao P,et al.2016.Microscopic evidence of new activities since late Quaternary in northern Suqian of Tancheng-Lujiang fault zone.Progress in Geophysics(in Chinese),31(3):1017-1026,doi:10.6038/pg20160312.
Yao D Q,Zheng H G,Zhao P,et al.2017.New activity of the Tanlu fault zone from Huaihe to the Nüshanhu since the late quaternary.Earthquake Research in China(in Chinese),33(1):38-45.
Yao H J,Van Der Hilst R D,De Hoop M V.2006.Surface-wave array tomography in SE Tibet from ambient seismic noise and two-station analysis-I.Phase velocity maps.Geophysical Journal International,166(2):732-744.
Yao H J,Van Der Hilst R D.2009.Analysis of ambient noise energy distribution and phase velocity bias in ambient noise tomography,with application to SE Tibet.Geophysical Journal International,179(2):1113-1132.
Yao H J,Van Der Hilst R D,Montagner J P.2010.Heterogeneity and anisotropy of the lithosphere of SE Tibet from surface wave array tomography.Journal of Geophysical Research:Solid Earth,115(B12):B12307,doi:10.1029/2009JB007142.
Yao H J,Gouedard P,Collins J A,et al.2011.Structure of young East Pacific Rise lithosphere from ambient noise correlation analysis of fundamental-and higher-mode Scholte-Rayleigh waves.Comptes Rendus Geoscience,343(8-9):571-583.
Zhang Y Y,Yan J,Liu X Q,et al.2017.Zircon age dating for dikes in the Yuexi area of Dabie Orogen and its significance.Journal of Mineralogy and Petrology(in Chinese),37(1):49-56.
Zhao P,Yao D Q,Yang Y Y,et al.2017a.The new activity of Tan-Lu fault zone in segment of Dahongshan since late quaternary.Seismology and Geology(in Chinese),39(3):550-560.
Zhao P,Yao D Q,Yang Y Y,et al.2017b.A new discovery of activity of Fushan section of the Tan-Lu fault zone in the late quaternary.Seismology and Geology(in Chinese),39(5):889-903.
Zhao T,Zhu G,Lin S Z,et al.2016.Indentation-induced tearing of a subducting continent:Evidence from the Tan-Lu fault zone,East China.Earth-Science Reviews,152:14-36.
Zhao Z F,Zheng Y F,Wei C S,et al.2004.Zircon U-Pb age,element and oxygen isotope geochemistry of mesozoic intermediatefelsic rocks in the Dabie mountains.Acta Petrologica Sinica(in Chinese),20(5):1151-1174.
Zhao Z F,Zheng Y F.2009.Remelting of subducted continental lithosphere:Petrogenesis of Mesozoic magmatic rocks in the Dabie-Sulu orogenic belt.Science in China Series D:Earth Sciences,52(9):1295-1318.
Zhao Z F,Zheng Y F,Dai L Q.2013.Origin of residual zircon and the nature of magma source for postcollisional granite in continental collision zone.Chinese Science Bulletin(in Chinese),58(23):2285-2289.
Zheng H G,Yao D Q,Zhao P,et al.2017.Preliminary study of macro and micro phenomenon of Late Quaternary new activities on Xujing Segment,Tancheng-Lujiang Fault Zone.Journal of Geodesy and Geodynamics(in Chinese),37(12):1219-1223.
Zheng L S,Gao W M,Zheng C B.1988.The segmentation of the Tan-Lu fault zone and activity in the Yishu fault zone.Earthquake Research in China(in Chinese),4(3):129-135.
Zheng X,Zhao C P,Zhou L Q,et al.2012.Rayleigh wave tomography from ambient noise in central and eastern Chinese mainland.Chinese Journal of Geophysics(in Chinese),55(6):1919-1928,doi:10.6038/j.issn.0001-5733.2012.06.013.
Zheng X F,Ouyang B,Zhang D N,et al.2009.Technical system construction of Data Backup Centre for China Seismograph Network and the data support to researches on the Wenchuan earthquake.Chinese Journal of Geophysics(in Chinese),52(5):1412-1417,doi:10.3969/j.issn.0001-5733.2009.05.031.
Zheng Y F,Fu B,Gong B,et al.2003.Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie-Sulu orogen in China:Implications for geodynamics and fluid regime.Earth-Science Reviews,62(1-2):105-161.
Zhou L Q,Xie J Y,Shen W S,et al.2012.The structure of the crust and uppermost mantle beneath South China from ambient noise and earthquake tomography.Geophysical Journal International,189(3):1565-1583.
Zhou T F,Fan Y,Yuan F,et al.2011.Petrogensis and metallogeny study of the volcanic basins in the Middle and Lower Yangtze metallogenic belt.Acta Geologica Sinica(in Chinese),85(5):712-730.
Zhu G,Niu M,Liu G,et al.2002a.Structural,magmatic and sedimentary events of the Tan-Lu fault belt during its Early Cretaceous strike-slip movement.Acta Geologica Sinica(in Chinese),76(3):325-334.
Zhu G,Song C Z,Niu M L,et al.2002b.Lithospheric textures of the Tan-Lu Fault Zone and their genetic analysis.Geological Journal of China Universities(in Chinese),8(3):248-256.
Zhu G,Wang D X,Liu G S,et al.2004.Evolution of the Tan-Lu fault zone and its responses to plate movements in west Pacific basin.Chinese Journal of Geology(in Chinese),39(1):36-49.
Zhu R X,Xu Y G,Zhu G,et al.2012.Destruction of the north China Craton.ScienceChinaEarthSciences,55(10):1565-1587.
常利军.2014.基于横波分裂、GPS和断裂第四纪滑动速率数据研究中国大陆及邻区岩石圈/软流圈动力学特征[博士论文].北京:中国地震局地球物理研究所.
从柏林,王清晨,张海政等.1996.中国合肥盆地新生代火山岩成因岩石学研究.岩石学报,12(3):370-381.
董树文,吴宣志,高锐等.1998.大别造山带地壳速度结构与动力学.地球物理学报,41(3):349-361.
黄耘,李清河,张元生等.2011.郯庐断裂带鲁苏皖段及邻区地壳速度结构.地球物理学报,54(10):2549-2559,doi:10.3969/j.issn.0001-5733.2011.10.012.
黄忠贤,胥颐,郝天珧等.2009.中国东部海域岩石圈结构面波层析成像.地球物理学报,52(3):653-662.
江国明,张贵宾,吕庆田等.2014.长江中下游地区成矿深部动力学机制:远震层析成像证据.岩石学报,30(4):907-917.
靳克,许文良,王清海等.2003.蚌埠淮光“混合花岗闪长岩”的形成时代及源区:锆石SHRIMP U-Pb地质年代学证据.地球学报,24(4):331-335.
林伟,王清晨,Faure M,Arnaud N.2005.从北淮阳构造带的多期变形透视大别山构造演化.中国科学D辑:地球科学,35(2):127-139.
刘福田,徐佩芬,刘劲松等.2003.大陆深俯冲带的地壳速度结构-东大别造山带深地震宽角反射/折射研究.地球物理学报,46(3):366-372.
刘晓强,闫峻,王爱国等.2016.大别造山带岳西地区中生代岩浆岩年代学研究.地质论评,62(4):897-914.
吕坚,谢祖军,郑勇等.2016.华南地块及其邻区Rayleigh波相速度层析成像研究.中国科学D辑:地球科学,46(11):1528-1541.
吕庆田,董树文,史大年等.2014.长江中下游成矿带岩石圈结构与成矿动力学模型---深部探测(SinoProbe)综述.岩石学报,30(4):889-906.
倪红玉,刘泽民,何康.2013.郯庐断裂带安徽段中小地震震源机制及现代应力场特征.地震工程学报,35(3):677-683.
欧阳龙斌,李红谊,吕庆田等.2015.长江中下游成矿带及邻区地壳剪切波速度结构和径向各向异性.地球物理学报,58(12):4388-4402,doi:10.6038/cjg20151205.
邱瑞龙,徐祥,黄德志.1999.华北陆块东南缘蚌埠地区荆山岩体同位素年龄及其地质意义.安徽地质,9(3):161-164.
王椿镛,张先康,丁志峰等.1997.大别造山带上部地壳结构的有限差分层析成像.地球物理学报,40(4):495-502.
王强,赵振华,熊小林等.2001.底侵玄武质下地壳的熔融:来自安徽沙溪adakite质富钠石英闪长玢岩的证据.地球化学,30(4):353-362.
王小凤,李中坚,陈柏林等.2005.郯庐断裂带.北京:地质出版社,12-13.
魏春景,张立飞,王式洸.2000.安徽省大别山东段中生代高钾花岗质岩石及其地质意义.中国科学(D辑),30(4):355-363.
吴萍萍,丁志峰,马小军等.2015.基于背景噪声研究大别-苏鲁及其邻区的瑞雷波群速度结构.地震学报,37(2):218-229.
熊振,李清河,张元生等.2016.郯庐断裂带鲁苏皖段地壳速度结构的分段特征及其地质意义.地球物理学报,59(7):2433-2443,doi:10.6038/cjg20160710.
徐嘉炜,崔可锐,朱光等.1984.中国东部郯庐断裂系统平移研究的若干进展.合肥工业大学学报,(2):28-37.
徐佩芬,孙若昧,刘福田等.1999.扬子板块俯冲、断离的地震层析成象证据.科学通报,44(15):1658-1661.
徐佩芬,刘福田,王清晨等.2000.大别-苏鲁碰撞造山带的地震层析成像研究-岩石圈三维速度结构.地球物理学报,43(3):377-385.
徐涛,张忠杰,田小波等.2014.长江中下游成矿带及邻区地壳速度结构:来自利辛-宜兴宽角地震资料的约束.岩石学报,30(4):918-930.
许文良,杨德彬,裴福萍等.2006.蚌埠隆起区五河杂岩的形成时代:锆石LA-ICP-MS U-Pb定年证据.中国地质,33(1):132-137.
杨德彬,许文良,裴福萍等.2005.蚌埠隆起区花岗岩形成时代及岩浆源区性质:锆石LA-ICPMS U-Pb定年与示踪.地球化学,34(5):443-454.
杨德彬,许文良,王清海等.2007.蚌埠隆起区中生代花岗岩的岩石成因:锆石Hf同位素的证据.岩石学报,23(2):381-392.
杨文采,胡振远,程振炎等.1999.郯城-涟水综合地球物理剖面.地球物理学报,42(2):206-217.
杨云,王维,王俊菲.2017.郯庐断裂带中南段应力场及变形特征.地震工程学报,39(S1):14-19.
杨源源,赵朋,郑海刚等.2017.郯庐断裂带安徽紫阳山段发现全新世活动证据.地震地质,39(4):644-655.
姚大全,杨源源,赵鹏等.2016.郯庐断裂带宿迁北晚第四纪以来新活动的微观证据.地球物理学进展,31(3):1017-1026,doi:10.6038/pg20160312.
姚大全,郑海刚,赵朋等.2017.郯庐断裂带淮河南到女山湖段晚第四纪以来的新活动.中国地震,33(1):38-45.
张媛媛,闫峻,刘晓强等.2017.大别造山带岳西地区岩脉群锆石定年及意义.矿物岩石,37(1):49-56.
赵朋,姚大全,杨源源等.2017a.郯庐断裂带大红山段晚第四纪以来的新活动.地震地质,39(3):550-560.
赵朋,姚大全,杨源源等.2017b.郯庐断裂带安徽浮山段晚第四纪以来活动新发现.地震地质,39(5):889-903.
赵子福,郑永飞,魏春生等.2004.大别山中生代中酸性岩浆岩锆石U-Pb定年、元素和氧同位素地球化学研究.岩石学报,20(5):1151-1174.
赵子福,郑永飞,戴立群.2013.大陆碰撞造山带花岗岩中继承锆石成因与岩浆源区性质.科学通报,58(23):2285-2289.
郑海刚,姚大全,赵朋等.2017.郯庐断裂带泗县徐井段晚第四纪新活动的宏微观现象初步研究.大地测量与地球动力学,37(12):1219-1223.
郑朗荪,高维明,郑传贝.1988.郯庐断裂带的分段与沂沭断裂的活动性.中国地震,4(3):129-135.
郑现,赵翠萍,周连庆等.2012.中国大陆中东部地区基于背景噪声的瑞利波层析成像.地球物理学报,55(6):1919-1928,doi:10.6038/j.issn.0001-5733.2012.06.013.
郑秀芬,欧阳飚,张东宁等.2009.“国家数字测震台网数据备份中心”技术系统建设及其对汶川大地震研究的数据支撑.地球物理学报,52(5):1412-1417,doi:10.3969/j.issn.0001-5733.2009.05.031.
周涛发,范裕,袁峰等.2011.长江中下游成矿带火山岩盆地的成岩成矿作用.地质学报,85(5):712-730.
朱光,牛漫兰,刘国生等.2002a.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件.地质学报,76(3):325-334.
朱光,宋传中,牛漫兰等.2002b.郯庐断裂带的岩石圈结构及其成因分析.高校地质学报,8(3):248-256.
朱光,王道轩,刘国生等.2004.郯庐断裂带的演化及其对西太平洋板块运动的响应.地质科学,39(1):36-49.
朱日祥,徐义刚,朱光等.2012.华北克拉通破坏.中国科学:地球科学,42(8):1135-1159.
Bensen G D,Ritzwoller M H,Shapiro N M.2008.Broadband ambient noise surface wave tomography across the United States.Journal of Geophysical Research:Solid Earth,113(B5):B05306,doi:10.1029/2007JB005248.
Chang L J.2014.Constraining the dynamic characteristics of lithosphere and asthenosphere in Mainland China and its adjacent regions using GPS,Quaternary fault slip rates and shear wave splitting data[Ph.D.thesis](in Chinese).Beijing:Institute of Geophysics,China Earthquake Administration.
Cong B L,Wang Q C,Zhang H Z,et al.1996.Petrogenesis of Cenozoic volcanic rocks in Hefei basin,China.Acta Petrologica Sinica(in Chinese),12(3):370-381.
Deng Y F,Fan W M,Zhang Z J,et al.2013.Geophysical evidence on segmentation of the Tancheng-Lujiang fault and its implications on the lithosphere evolution in East China.Journal of Asian Earth Sciences,2013,78:263-276.
Dong S W,Wu X Z,Gao R,et al.1998.On the crust velocity levels and dynamics of the Dabieshan orogenic belt.Acta Geophysica Sinica(in Chinese),41(3):349-361.
Hacker B R,Ratschbacher L,Webb L,et al.1998.U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling-Dabie Orogen,China.Earth and Planetary Science Letters,161(1-4):215-230.
Hacker B R,Ratschbacher L,Liou J G.2004.Subduction,collision and exhumation in the ultrahigh-pressure Qinling-Dabie orogen.Geological Society,London,Special Publications,2004,226(1):157-175.
He R Z,Shang X F,Yu C Q,et al.2014.A unified map of Moho depth and VP/VSratio of continental China by receiver function analysis.Geophysical Journal International,199(3):1910-1918.
Herrmann R B,Ammon C J.2002.Surface Waves,Receiver Functions and Crustal Structure,Computer Programs in Seismology,version3.30.Saint Louis:Saint Louis University.
Huang J L,Zhao D P.2006.High-resolution mantle tomography of China and surrounding regions.Journal of Geophysical Research:Solid Earth,111(B9):B09305,doi:10.1029/2005JB004066.
Huang R,Xu Y X,Zhu L P,et al.2015.Detailed Moho geometry beneath southeastern China and its implications on thinning of continental crust.Journal of Asian Earth Sciences,112:42-48.
Huang Y,Li Q H,Zhang Y S,et al.2011.Crustal velocity structure beneath the Shandong-Jiangsu-Anhui segment of the TanchengLujiang Fault Zone and adjacent areas.Chinese Journal of Geophysics(in Chinese),54(10):2549-2559,doi:10.3969/j.issn.0001-5733.2011.10.012.
Huang Z X,Su W,Peng Y J,et al.2003.Rayleigh wave tomography of China and adjacent regions.Journal of Geophysical Research:Solid Earth,108(B2):2073,doi:10.1029/2001JB001696.
Huang Z X,Xu Y,Hao T Y,et al.2009.Surface wave tomography of lithospheric structure in the seas of east China.Chinese Journal of Geophysics(in Chinese),52(3):653-662.
Jiang G M,Zhang G B,Lv Q T,et al.2013.3-D velocity model beneath the Middle-Lower Yangtze River and its implication to the deep geodynamics.Tectonophysics,606:36-47.
Jiang G M,Zhang G B,Lu Q T,et al.2014.Deep geodynamics of mineralization beneath the Middle-Lower Reaches of Yangtze River:Evidence from teleseismic tomography.Acta Petrologica Sinica(in Chinese),30(4):907-917.
Jin K,Xu W L,Wang Q H,et al.2003.Formation time and sources of the Huaiguang“Migmatitic Granodiorite”in Bengbu,Anhui Province:Evidence from SHRIMP zircon U-Pb geochronology.Acta Geoscientia Sinica(in Chinese),24(4):331-335.
LüJ,Xie Z J,Zheng Y,et al.2016.Rayleigh wave phase velocities of South China block and its adjacent areas.Science in China Earth Sciences,59(11):2165-2178.
LüQ T,Dong S W,Shi D N,et al.2014.Lithosphere architecture and geodynamic model of middle and lower reaches of Yangtze metallogenic belt:A review from SinoProbe.Acta Petrologica Sinica(in Chinese),30(4):889-906.
Leary P C,Crampin S,McEvilly T V.1990.Seismic fracture anisotropy in the Earth′s crust:An overview.Journal of Geophysical Research:Solid Earth,95(B7):11105-11114.
Li S Q,Chen F K,Siebel W,et al.2012.Late Mesozoic tectonic evolution of the Songliao basin,NE China:Evidence from detrital zircon ages and Sr-Nd isotopes.Gondwana Research,22(3-4):943-955.
Li S Z,Kusky T M,Zhao G C,et al.2010.Two-stage Triassic exhumation of HP-UHP terranes in the western Dabie orogen of China:Constraints from structural geology.Tectonophysics,490(3-4):267-293.
Lin W,Michel F,Wang Q C,et al.2005.Tectonic evolution of the Dabieshan orogen:In the view from polyphase deformation of the Beihuaiyang metamorphic zone.Science in China Series D:Earth Sciences,48(7):886-899.
Liu C M,Yao H J.2017.Surface wave tomography with spatially varying smoothing based on continuous model regionalization.Pure and Applied Geophysics,174(3):937-953.
Liu F T,Xu P F,Liu J S,et al.2003.The crustal velocity structure of the continental deep subduction belt:Study on the eastern Dabie orogen by seismic wide-angle reflection/refraction.Chinese Journal of Geophysics(in Chinese),46(3):366-372.
Liu S A,Li S G,Guo S S,et al.2012.The Cretaceous adakiticbasaltic-granitic magma sequence on south-eastern margin of the North China Craton:Implications for lithospheric thinning mechanism.Lithos,134-135:163-178.
Liu X Q,Yan J,Wang A G,et al.2016.Geochronological study on Mesozoic magmatic rocks in Yuexi area,Dabie Orogen.Geological Review(in Chinese),62(4):897-914.
Luo Y H,Xu Y X,Yang Y J.2012.Crustal structure beneath the Dabie orogenic belt from ambient noise tomography.Earth and Planetary Science Letters,313-314:12-22.
Luo Y H,Xu Y X,Yang Y J.2013.Crustal radial anisotropy beneath the Dabie orogenic belt from ambient noise tomography.Geophysical Journal International,195(2):1149-1164.
Montagner J P,Nataf H C.1986.A simple method for inverting the azimuthal anisotropy of surface waves.Journal of Geophysical Research:Solid Earth,91(B1):511-520.
Nafe J E,Drake C L.1957.Variation with depth in shallow and deep water marine sediments of porosity,density and the velocities of compressional and shear waves.Geophysics,22(3):523-713.
Ni H Y,Liu Z M,He K.2013.Study on focal mechanisms of moderatesmall earthquakes and characteristics of recent tectonic stress field in the Anhui sector of Tanlu fault zone.China Earthquake Engineering Journal(in Chinese),35(3):677-683.
Ouyang L B,Li H Y,Lv Q T,et al.2014.Crustal and uppermost mantle velocity structure and its relationship with the formation of ore districts in the Middle-Lower Yangtze River region.Earth and Planetary Science Letters,408:378-389.
Ouyang L B,Li H Y,LüQ T,et al.2015.Crustal shear wave velocity structure and radial anisotropy beneath the MiddleLower Yangtze River metallogenic belt and surrounding areas from seismic ambient noise tomography.Chinese Journal of Geophysics(in Chinese),58(12):4388-4402,doi:10.6038/cjg20151205.
Qiu R L,Xu X,Huang D Z.1999.The isotopic age of the Jingshan intrusive in the Bengbu region of the southeastern edge of the north china block and its geological implications.Geology of Anhui(in Chinese),9(3):161-164.
Shen W S,Ritzwoller M H,Kang D,et al.2016.A seismic reference model for the crust and uppermost mantle beneath China from surface wave dispersion.Geophysical Journal International,206(2):954-979.
Shi D N,LüQ T,Xu W Y,et al.2013.Crustal structure beneath the middle-lower Yangtze metallogenic belt in East China:Constraints from passive source seismic experiment on the Mesozoic intra-continental mineralization.Tectonophysics,606:48-59.
Tarantola A,Valette B.1982.Generalized nonlinear inverse problems solved using the least squares criterion.Review of Geophysics,20(2):219-232.
Wang C Y,Zhang X K,Ding Z F,et al.1997.Finite-difference tomography of upper crustal structure in Dabieshan orogenic belt.Acta Geophysica Sinica(in Chinese),40(4):495-502.
Wang Q,Zhao Z H,Xiong X L,et al.2001.Melting of the underplated basaltic lower crust:Evidence from the Shaxi adakitic sodic quartz diorite-porphyrites,Anhui Province,China.Geochimica(in Chinese),30(4):353-362.
Wang X F,Li Z J,Chen B L,et al.2005.On the Tan-Lu Fault Zone(in Chinese).Beijing:Geological Publishing House,12-13.
Wang Y J,Fan W M,Peng T P,et al.2005.Nature of the Mesozoic lithospheric mantle and tectonic decoupling beneath the Dabie Orogen,Central China:Evidence from 40 Ar/39 Ar geochronology,elemental and Sr-Nd-Pb isotopic compositions of early Cretaceous mafic igneous rocks.Chemical Geology,220(3-4):165-189.
Wei C J,Zhang L F,Wang S G.2001.Mesozoic high-K granitic rocks from the eastern Dabie Mountains,Central China and their geological implications.Science in China Series D:Earth Sciences,44(6):525-534.
Weiss T,Siegesmund S,Rabbel W,et al.1999.Seismic velocities and anisotropy of the lower continental crust:A review.Pure and Applied Geophysics,156(1-2):97-122.
Wu P P,Ding Z F,Ma X J,et al.2015.Rayleigh wave group velocity tomography beneath Dabie-Sulu and its adjacent areas from ambient seismic noise.Acta Seismologica Sinica(in Chinese),37(2):218-229.
Xie Z,Zheng Y F,Zhao Z F,et al.2006.Mineral isotope evidence for the contemporaneous process of Mesozoic granite emplacement and gneiss metamorphism in the Dabie orogen.Chemical Geology,231(3):214-235.
Xiong Z,LI Q H,Zhang Y S,et al.2016.Segmentation of crustal velocity structure beneath the Shandong-Jiangsu-Anhui segment of the Tanlu fault zone and adjacent areas and its geological implications.Chinese Journal of Geophysics(in Chinese),59(7):2433-2443,doi:10.6038/cjg20160710.
Xu J F,Shinjo R,Defant M J,et al.2002.Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China:Partial melting of delaminated lower continental crust?.Geology,30(12):1111-1114.
Xu J W,Cui K R,Zhu G,et al.1984.Some progress of displacement research of the Tan-Lu fault system,eastern China.Journal of Hefei Polytechnic University(in Chinese),(2):28-37.
Xu P F,Sun R M,Liu Fu T,et al.2000.Seismic tomography showing subduction and slab breakoff of the Yangtze block beneath the Dabie-Sulu orogenic belt.Chinese Science Bulletin,44(1):70-74.
Xu P F,Liu F T,Wang Q C,et al.2000.Seismic tomography beneath the Dabie-Sulu collision orogen 3-D velocity structures of lithosphere.Chinese Journal of Geophysics(in Chinese),43(3):377-385.
Xu T,Zhang Z J,Tian X B,et al.2014.Crustal structure beneath the Middle-Lower Yangtze metallogenic belt and its surrounding areas:Constraints from active source seismic experiment along the Lixin to Yixing profile in East China.Acta Petrologica Sinica(in Chinese),30(4):918-930.
Xu W L,Wang Q H,Yang D B,et al.2005.SHRIMP zircon U-Pb dating in Jingshan“migmatitic granite”,Bengbu and its geological significance.Science in China Series D:Earth Sciences,48(2):185-191.
Xu W L,Yang D B,Pei F P,et al.2006.Age of the Wuhe complex in the Bengbu uplift:Evidence from LA-ICP-MS zircon U-Pb dating.Geology in China(in Chinese),33(1):132-137.
Yang D B,Xu W L,Pei F P,et al.2005.Formation time and magma source of granites in Bengbu uplift:Evidence from LA-ICPMS zircon U-Pb dating and tracing.Geochimica(in Chinese),34(5):443-454.
Yang D B,Xu W L,Wang Q H,et al.2007.Petrogenesis of the Mesozoic granite in Bengbu uplift:Constraints from zircon Hf isotope.Acta Petrologica Sinica(in Chinese),23(2):381-392.
Yang W C,Hu Z Y,Cheng Z Y,et al.1999.Long profile of geophysical investigation from Tanchen to Lianshui,East-Central China.Chinese Journal of Geophysics(in Chinese),42(2):206-217.
Yang W C.2002.Geophysical profiling across the Sulu ultra-highpressure metamorphic belt,eastern China.Tectonophysics,354(3-4):277-288.
Yang Y,Wang W,Wang J F.2017.Characteristics of regional stress field and latest crustal deformation in middle-southern segment of Tan-Lu fault zone.China Earthquake Engineering Journal(in Chinese),39(S1):14-19.
Yang Y Y,Zhao P,Zheng H G,et al.2017.Evidence of holocene activity discovered in anhui ziyangshan segment of tanlu fault zone.Seismology and Geology(in Chinese),39(4):644-655.
Yao D Q,Yang Y Y,Zhao P,et al.2016.Microscopic evidence of new activities since late Quaternary in northern Suqian of Tancheng-Lujiang fault zone.Progress in Geophysics(in Chinese),31(3):1017-1026,doi:10.6038/pg20160312.
Yao D Q,Zheng H G,Zhao P,et al.2017.New activity of the Tanlu fault zone from Huaihe to the Nüshanhu since the late quaternary.Earthquake Research in China(in Chinese),33(1):38-45.
Yao H J,Van Der Hilst R D,De Hoop M V.2006.Surface-wave array tomography in SE Tibet from ambient seismic noise and two-station analysis-I.Phase velocity maps.Geophysical Journal International,166(2):732-744.
Yao H J,Van Der Hilst R D.2009.Analysis of ambient noise energy distribution and phase velocity bias in ambient noise tomography,with application to SE Tibet.Geophysical Journal International,179(2):1113-1132.
Yao H J,Van Der Hilst R D,Montagner J P.2010.Heterogeneity and anisotropy of the lithosphere of SE Tibet from surface wave array tomography.Journal of Geophysical Research:Solid Earth,115(B12):B12307,doi:10.1029/2009JB007142.
Yao H J,Gouedard P,Collins J A,et al.2011.Structure of young East Pacific Rise lithosphere from ambient noise correlation analysis of fundamental-and higher-mode Scholte-Rayleigh waves.Comptes Rendus Geoscience,343(8-9):571-583.
Zhang Y Y,Yan J,Liu X Q,et al.2017.Zircon age dating for dikes in the Yuexi area of Dabie Orogen and its significance.Journal of Mineralogy and Petrology(in Chinese),37(1):49-56.
Zhao P,Yao D Q,Yang Y Y,et al.2017a.The new activity of Tan-Lu fault zone in segment of Dahongshan since late quaternary.Seismology and Geology(in Chinese),39(3):550-560.
Zhao P,Yao D Q,Yang Y Y,et al.2017b.A new discovery of activity of Fushan section of the Tan-Lu fault zone in the late quaternary.Seismology and Geology(in Chinese),39(5):889-903.
Zhao T,Zhu G,Lin S Z,et al.2016.Indentation-induced tearing of a subducting continent:Evidence from the Tan-Lu fault zone,East China.Earth-Science Reviews,152:14-36.
Zhao Z F,Zheng Y F,Wei C S,et al.2004.Zircon U-Pb age,element and oxygen isotope geochemistry of mesozoic intermediatefelsic rocks in the Dabie mountains.Acta Petrologica Sinica(in Chinese),20(5):1151-1174.
Zhao Z F,Zheng Y F.2009.Remelting of subducted continental lithosphere:Petrogenesis of Mesozoic magmatic rocks in the Dabie-Sulu orogenic belt.Science in China Series D:Earth Sciences,52(9):1295-1318.
Zhao Z F,Zheng Y F,Dai L Q.2013.Origin of residual zircon and the nature of magma source for postcollisional granite in continental collision zone.Chinese Science Bulletin(in Chinese),58(23):2285-2289.
Zheng H G,Yao D Q,Zhao P,et al.2017.Preliminary study of macro and micro phenomenon of Late Quaternary new activities on Xujing Segment,Tancheng-Lujiang Fault Zone.Journal of Geodesy and Geodynamics(in Chinese),37(12):1219-1223.
Zheng L S,Gao W M,Zheng C B.1988.The segmentation of the Tan-Lu fault zone and activity in the Yishu fault zone.Earthquake Research in China(in Chinese),4(3):129-135.
Zheng X,Zhao C P,Zhou L Q,et al.2012.Rayleigh wave tomography from ambient noise in central and eastern Chinese mainland.Chinese Journal of Geophysics(in Chinese),55(6):1919-1928,doi:10.6038/j.issn.0001-5733.2012.06.013.
Zheng X F,Ouyang B,Zhang D N,et al.2009.Technical system construction of Data Backup Centre for China Seismograph Network and the data support to researches on the Wenchuan earthquake.Chinese Journal of Geophysics(in Chinese),52(5):1412-1417,doi:10.3969/j.issn.0001-5733.2009.05.031.
Zheng Y F,Fu B,Gong B,et al.2003.Stable isotope geochemistry of ultrahigh pressure metamorphic rocks from the Dabie-Sulu orogen in China:Implications for geodynamics and fluid regime.Earth-Science Reviews,62(1-2):105-161.
Zhou L Q,Xie J Y,Shen W S,et al.2012.The structure of the crust and uppermost mantle beneath South China from ambient noise and earthquake tomography.Geophysical Journal International,189(3):1565-1583.
Zhou T F,Fan Y,Yuan F,et al.2011.Petrogensis and metallogeny study of the volcanic basins in the Middle and Lower Yangtze metallogenic belt.Acta Geologica Sinica(in Chinese),85(5):712-730.
Zhu G,Niu M,Liu G,et al.2002a.Structural,magmatic and sedimentary events of the Tan-Lu fault belt during its Early Cretaceous strike-slip movement.Acta Geologica Sinica(in Chinese),76(3):325-334.
Zhu G,Song C Z,Niu M L,et al.2002b.Lithospheric textures of the Tan-Lu Fault Zone and their genetic analysis.Geological Journal of China Universities(in Chinese),8(3):248-256.
Zhu G,Wang D X,Liu G S,et al.2004.Evolution of the Tan-Lu fault zone and its responses to plate movements in west Pacific basin.Chinese Journal of Geology(in Chinese),39(1):36-49.
Zhu R X,Xu Y G,Zhu G,et al.2012.Destruction of the north China Craton.ScienceChinaEarthSciences,55(10):1565-1587.
常利军.2014.基于横波分裂、GPS和断裂第四纪滑动速率数据研究中国大陆及邻区岩石圈/软流圈动力学特征[博士论文].北京:中国地震局地球物理研究所.
从柏林,王清晨,张海政等.1996.中国合肥盆地新生代火山岩成因岩石学研究.岩石学报,12(3):370-381.
董树文,吴宣志,高锐等.1998.大别造山带地壳速度结构与动力学.地球物理学报,41(3):349-361.
黄耘,李清河,张元生等.2011.郯庐断裂带鲁苏皖段及邻区地壳速度结构.地球物理学报,54(10):2549-2559,doi:10.3969/j.issn.0001-5733.2011.10.012.
黄忠贤,胥颐,郝天珧等.2009.中国东部海域岩石圈结构面波层析成像.地球物理学报,52(3):653-662.
江国明,张贵宾,吕庆田等.2014.长江中下游地区成矿深部动力学机制:远震层析成像证据.岩石学报,30(4):907-917.
靳克,许文良,王清海等.2003.蚌埠淮光“混合花岗闪长岩”的形成时代及源区:锆石SHRIMP U-Pb地质年代学证据.地球学报,24(4):331-335.
林伟,王清晨,Faure M,Arnaud N.2005.从北淮阳构造带的多期变形透视大别山构造演化.中国科学D辑:地球科学,35(2):127-139.
刘福田,徐佩芬,刘劲松等.2003.大陆深俯冲带的地壳速度结构-东大别造山带深地震宽角反射/折射研究.地球物理学报,46(3):366-372.
刘晓强,闫峻,王爱国等.2016.大别造山带岳西地区中生代岩浆岩年代学研究.地质论评,62(4):897-914.
吕坚,谢祖军,郑勇等.2016.华南地块及其邻区Rayleigh波相速度层析成像研究.中国科学D辑:地球科学,46(11):1528-1541.
吕庆田,董树文,史大年等.2014.长江中下游成矿带岩石圈结构与成矿动力学模型---深部探测(SinoProbe)综述.岩石学报,30(4):889-906.
倪红玉,刘泽民,何康.2013.郯庐断裂带安徽段中小地震震源机制及现代应力场特征.地震工程学报,35(3):677-683.
欧阳龙斌,李红谊,吕庆田等.2015.长江中下游成矿带及邻区地壳剪切波速度结构和径向各向异性.地球物理学报,58(12):4388-4402,doi:10.6038/cjg20151205.
邱瑞龙,徐祥,黄德志.1999.华北陆块东南缘蚌埠地区荆山岩体同位素年龄及其地质意义.安徽地质,9(3):161-164.
王椿镛,张先康,丁志峰等.1997.大别造山带上部地壳结构的有限差分层析成像.地球物理学报,40(4):495-502.
王强,赵振华,熊小林等.2001.底侵玄武质下地壳的熔融:来自安徽沙溪adakite质富钠石英闪长玢岩的证据.地球化学,30(4):353-362.
王小凤,李中坚,陈柏林等.2005.郯庐断裂带.北京:地质出版社,12-13.
魏春景,张立飞,王式洸.2000.安徽省大别山东段中生代高钾花岗质岩石及其地质意义.中国科学(D辑),30(4):355-363.
吴萍萍,丁志峰,马小军等.2015.基于背景噪声研究大别-苏鲁及其邻区的瑞雷波群速度结构.地震学报,37(2):218-229.
熊振,李清河,张元生等.2016.郯庐断裂带鲁苏皖段地壳速度结构的分段特征及其地质意义.地球物理学报,59(7):2433-2443,doi:10.6038/cjg20160710.
徐嘉炜,崔可锐,朱光等.1984.中国东部郯庐断裂系统平移研究的若干进展.合肥工业大学学报,(2):28-37.
徐佩芬,孙若昧,刘福田等.1999.扬子板块俯冲、断离的地震层析成象证据.科学通报,44(15):1658-1661.
徐佩芬,刘福田,王清晨等.2000.大别-苏鲁碰撞造山带的地震层析成像研究-岩石圈三维速度结构.地球物理学报,43(3):377-385.
徐涛,张忠杰,田小波等.2014.长江中下游成矿带及邻区地壳速度结构:来自利辛-宜兴宽角地震资料的约束.岩石学报,30(4):918-930.
许文良,杨德彬,裴福萍等.2006.蚌埠隆起区五河杂岩的形成时代:锆石LA-ICP-MS U-Pb定年证据.中国地质,33(1):132-137.
杨德彬,许文良,裴福萍等.2005.蚌埠隆起区花岗岩形成时代及岩浆源区性质:锆石LA-ICPMS U-Pb定年与示踪.地球化学,34(5):443-454.
杨德彬,许文良,王清海等.2007.蚌埠隆起区中生代花岗岩的岩石成因:锆石Hf同位素的证据.岩石学报,23(2):381-392.
杨文采,胡振远,程振炎等.1999.郯城-涟水综合地球物理剖面.地球物理学报,42(2):206-217.
杨云,王维,王俊菲.2017.郯庐断裂带中南段应力场及变形特征.地震工程学报,39(S1):14-19.
杨源源,赵朋,郑海刚等.2017.郯庐断裂带安徽紫阳山段发现全新世活动证据.地震地质,39(4):644-655.
姚大全,杨源源,赵鹏等.2016.郯庐断裂带宿迁北晚第四纪以来新活动的微观证据.地球物理学进展,31(3):1017-1026,doi:10.6038/pg20160312.
姚大全,郑海刚,赵朋等.2017.郯庐断裂带淮河南到女山湖段晚第四纪以来的新活动.中国地震,33(1):38-45.
张媛媛,闫峻,刘晓强等.2017.大别造山带岳西地区岩脉群锆石定年及意义.矿物岩石,37(1):49-56.
赵朋,姚大全,杨源源等.2017a.郯庐断裂带大红山段晚第四纪以来的新活动.地震地质,39(3):550-560.
赵朋,姚大全,杨源源等.2017b.郯庐断裂带安徽浮山段晚第四纪以来活动新发现.地震地质,39(5):889-903.
赵子福,郑永飞,魏春生等.2004.大别山中生代中酸性岩浆岩锆石U-Pb定年、元素和氧同位素地球化学研究.岩石学报,20(5):1151-1174.
赵子福,郑永飞,戴立群.2013.大陆碰撞造山带花岗岩中继承锆石成因与岩浆源区性质.科学通报,58(23):2285-2289.
郑海刚,姚大全,赵朋等.2017.郯庐断裂带泗县徐井段晚第四纪新活动的宏微观现象初步研究.大地测量与地球动力学,37(12):1219-1223.
郑朗荪,高维明,郑传贝.1988.郯庐断裂带的分段与沂沭断裂的活动性.中国地震,4(3):129-135.
郑现,赵翠萍,周连庆等.2012.中国大陆中东部地区基于背景噪声的瑞利波层析成像.地球物理学报,55(6):1919-1928,doi:10.6038/j.issn.0001-5733.2012.06.013.
郑秀芬,欧阳飚,张东宁等.2009.“国家数字测震台网数据备份中心”技术系统建设及其对汶川大地震研究的数据支撑.地球物理学报,52(5):1412-1417,doi:10.3969/j.issn.0001-5733.2009.05.031.
周涛发,范裕,袁峰等.2011.长江中下游成矿带火山岩盆地的成岩成矿作用.地质学报,85(5):712-730.
朱光,牛漫兰,刘国生等.2002a.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件.地质学报,76(3):325-334.
朱光,宋传中,牛漫兰等.2002b.郯庐断裂带的岩石圈结构及其成因分析.高校地质学报,8(3):248-256.
朱光,王道轩,刘国生等.2004.郯庐断裂带的演化及其对西太平洋板块运动的响应.地质科学,39(1):36-49.
朱日祥,徐义刚,朱光等.2012.华北克拉通破坏.中国科学:地球科学,42(8):1135-1159.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |