利用接收函数方法研究中国东北东南部地区不同构造体的地壳特征
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摘要
基于我们布设的探测深俯冲的中国东北地震台阵NECsaids台阵和固定地震台长时段的观测记录及NECESSArray流动台阵共计152个台站数据提取得到的33752条P波接收函数,采用H-κ叠加分析和共转换点(CCP)叠加成像等方法进行统一分析处理,并汇集他人接收函数研究结果得到中国东北东南部地区迄今为止最高分辨率的地壳厚度和平均波速比分布图像.对中国东北东南部地区不同构造体的地壳特征综合分析研究表明:研究区不同陆块的地壳属性存在明显差别,张广才岭地块中南部的地壳厚度和波速比与华北克拉通东北缘相当,地壳厚度同地表地形之间显示有明显的正相关关系;松辽地块东南缘地壳最薄、波速比最高,地壳厚度同壳内波速比之间显示出明显的负相关关系;兴凯地块西部地区的地壳结构表现为稍厚的地壳厚度和研究区内最低的壳内波速比,其地壳厚度同壳内波速比之间亦显示出明显的负相关关系;佳木斯地块西南缘在具有"正常"的壳内波速比同时地壳最厚.研究区内的郯庐断裂带北延段在切穿其下Moho面的同时表现出南北分段的特征:北段(44.4°N—47°N)两分支之下的Moho面整体下凹,而南段(41.5°N—43.3°N)两分支之下的Moho面则整体上隆.长白山天池火山下方表现为Moho面下凹沉落及高壳内波速比特征,推测其壳内岩浆囊很可能存在于火山口东北隅至少10km的范围内.
Based on our broadband seismological records named NECsaids(NorthEast China Seismic Array to Investigate Deep Subduction)that deployed in NE China from July 2010 to May2017,as well as the permanent seismological records operated by China Earthquake Administration(CEA)from August 2007 to May 2017 and seismological records from the international collaborative project named NECESSArray(NorthEast China Extended Seismic Array)from September 2009 to August 2011,we acquired 33752 P-wave receiver functions(RFs)in total with high quality.And then using H-κstacking technique and common converted points(CCP)stacking technique,we obtained the highest-resolution crustal structure in southeastern part of NE China so far as we know,which consists of 231 measurements of crustal thickness and VP/VSratio(including 89 measurements from former studies)and 3 CCP stacking profiles.The main results in this study are summarized as follow:The five micro-continental blocks in our study region show different crustal structure distinctly.The south-central part of the Zhangguangcai Ranges owns the similar crustal thickness and VP/VS ratio as the northeastern part of the North China Craton.The southeastern part of the Songliao Block has the thinnest crust and highest crustal VP/VSratio.As for the western Khanka Block,it keeps a slightly thicker crustal thickness while with the lowest crustal VP/VSratio.The southwestern part of the Jiamusi Massif owns an ordinary crustal VP/VSratio but its crust is the thickest.The important tectonic line like the Tanlu Fault Zone which in depth cut through the Moho discontinuity,its northern segment appears to have different crustal structure in its northern and southern parts.For its northern part(44.4°N—47°N),the Moho discontinuity between the two main branches appears to drop down.While for the southern part(41.5°N—43.3°N),the Moho discontinuity changes into being uplifted under the fault zone.Around the Changbaishan Tianchi volcano,the Moho discontinuity under the caldera subsides and the measurements at 3 stations(2 measurements cited from former study)with high VP/VSratio located at the north and east of the caldera within10 km may indicate the present crustal magma.
Based on our broadband seismological records named NECsaids(NorthEast China Seismic Array to Investigate Deep Subduction)that deployed in NE China from July 2010 to May2017,as well as the permanent seismological records operated by China Earthquake Administration(CEA)from August 2007 to May 2017 and seismological records from the international collaborative project named NECESSArray(NorthEast China Extended Seismic Array)from September 2009 to August 2011,we acquired 33752 P-wave receiver functions(RFs)in total with high quality.And then using H-κstacking technique and common converted points(CCP)stacking technique,we obtained the highest-resolution crustal structure in southeastern part of NE China so far as we know,which consists of 231 measurements of crustal thickness and VP/VSratio(including 89 measurements from former studies)and 3 CCP stacking profiles.The main results in this study are summarized as follow:The five micro-continental blocks in our study region show different crustal structure distinctly.The south-central part of the Zhangguangcai Ranges owns the similar crustal thickness and VP/VS ratio as the northeastern part of the North China Craton.The southeastern part of the Songliao Block has the thinnest crust and highest crustal VP/VSratio.As for the western Khanka Block,it keeps a slightly thicker crustal thickness while with the lowest crustal VP/VSratio.The southwestern part of the Jiamusi Massif owns an ordinary crustal VP/VSratio but its crust is the thickest.The important tectonic line like the Tanlu Fault Zone which in depth cut through the Moho discontinuity,its northern segment appears to have different crustal structure in its northern and southern parts.For its northern part(44.4°N—47°N),the Moho discontinuity between the two main branches appears to drop down.While for the southern part(41.5°N—43.3°N),the Moho discontinuity changes into being uplifted under the fault zone.Around the Changbaishan Tianchi volcano,the Moho discontinuity under the caldera subsides and the measurements at 3 stations(2 measurements cited from former study)with high VP/VSratio located at the north and east of the caldera within10 km may indicate the present crustal magma.
引文
Amante C,Eakins B W.2009.ETOPO1 1Arc-Minute Global Relief Model:procedures,data sources and analysis.NOAA Technical Memorandum NESDIS NGDC-24.National Geophysical Data Center,NOAA.
Chen L,Zheng T Y,Xu W W.2006.A thinned lithospheric image of the Tanlu Fault Zone,eastern China:Constructed from wave equation based receiver function migration.Journal of Geophysical Research:Solid Earth,111(B9):B09312,doi:10.1029/2005JB003974.
Chen Y L,Niu F L,Liu R F,et al.2010.Crustal structure beneath China from receiver function analysis.Journal of Geophysical Research:Solid Earth,115(B3):B03307,doi:10.1029/2009JB006386.
Cheng S Y.2006.Regional tectonic characters and Meso-Cenozoic basin evolution in Northeastern China[Ph.D.thesis](in Chinese).Beijing:China University of Geosciences,Beijing.
Data Management Centre of China National Seismic Network.2007-05-23.Waveform data of China National Seismic Network.Institute of Geophysics,China Earthquake Administration,http:∥www.seisdmc.ac.cn.
DeMets C,Gordon R G,Argus D F,et al.1994.Effect of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions.Geophysical Research Letters,21(20):2191-2194.
Deng J F,Mo X X,Zhao H L,et al.1994.Lithosphere root/derooting and activation of the east China continent.Geoscience(in Chinese),8(3):349-356.
Deng Q D,Zhang P Z,Ran Y K,et al.2003.Active tectonics and earthquake activities in China.Earth Science Frontiers(in Chinese),10(S1):66-73.
Duan Y H,Zhang X K,Liu Z,et al.2005.A study on crustal structures of Changbaishan-Jingpohu volcanic area using receiver functions.Chinese Journal of Geophysics(in Chinese),48(2):352-358.
Dueker K G,Sheehan A F.1997.Mantle discontinuity structure from midpoint stacks of converted P to S waves across the Yellowstone hotspot track.Journal of Geophysical Research:Solid Earth,102(B4):8313-8327.
Efron B,Tibshirani R.1986.Bootstrap methods for standard errors,confidence intervals,and other measures of statistical accuracy.Statistical Science,1(1):54-75.
Fan Q C,Sui J L,Wang T H,et al.2007.History of volcanic activity,magma evolution and eruptive mechanisms of the Changbai volcanic province.Geological Journal of China Universities(in Chinese),13(2):175-190.
Gao Z Y.2015.The study of the crustal and upper mantle structure in Northeast China from teleseismic receiver function[Master′s thesis](in Chinese).Beijing:Institute of Geophysics,China Earthquake Administration.
Guo M X,Sun W,Yin G Y,et al.2000.North-extension of the Tanlu fracture and geologic-geophysical characteristics.Jilin Geology(in Chinese),19(3):35-44.
Guo Z,Tang Y C,Chen John,et al.2012.A study on crustal and upper mantle structures in east part of North China Craton using receiver functions.Chinese Journal of Geophysics(in Chinese),55(11):3591-3600,doi:10.6038/j.issn.0001-5733.2012.11.008.
Guo Z,Chen Y J,Ning J Y,et al.2015.High resolution 3-Dcrustal structure beneath NE China from joint inversion of ambient noise and receiver functions using NECESSArray data.Earth and Planetary Science Letters,416:1-11.
Guo Z,Chen Y J,Ning J Y,et al.2016.Seismic evidence of ongoing sublithosphere upper mantle convection for intra-plate volcanism in Northeast China.Earth and Planetary Science Letters,433:31-43.
He C S,Dong S W,Santosh M,et al.2013.Seismic evidence for a geosuture between the Yangtze and Cathaysia Blocks,South China.Scientific Reports,3:2200.
He R Z,Shan 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.
Hetland E A,Wu F T,Song J L.2004.Crustal structure in the Changbaishan volcanic area,China,determined by modeling receiver functions.Tectonophysics,386(3-4):157-175.
Ji S C,Wang X,Yang W C.2009.Correlation between crustal thickness and Poisson′s ratio in the North China Craton and its implication for lithospheric thinning.Acta Geologica Sinica(in Chinese),83(3):324-330.
Kennett B L N,Engdahl E R.1991.Traveltimes for global earthquake location and phase identification.Geophysical Journal International,105(2):429-465.
Kind R,Yuan X H,Kumar P.2012.Seismic receiver functions and the lithosphere-asthenosphere boundary.Tectonophysics,536-537:25-43.
Kyong-Song R,Hammond J O S,Chol-Nam K,et al.2016.Evidence for partial melt in the crust beneath Mt.Paektu(Changbaishan),Democratic People′s Republic of Korea and China.Science Advances,2(4):e1501513.
Langston C A.1979.Structure under Mount Rainier,Washington,inferred from teleseismic body waves.Journal of Geophysical Research:Solid Earth,84(B9):4749-4762.
Li K,Liu J Q,Pan X D,et al.2009.Crust deformation monitoring and research in Tianchi volcanic area,Changbai mountains from 2000-2007.Seismology and Geology(in Chinese),31(4):639-646.
Li X F,Chen Q M,Zhang X H,et al.2002.The Yitong grabenthe structural features and evolution of a strike-slip fault basin.Petroleum Geology&Experiment(in Chinese),24(1):19-30.
Li Y H,Wu Q J,Pan J T,et al.2012.S-wave velocity structure of northeastern China from joint inversion of Rayleigh wave phase and group velocities.Geophysical Journal International,190(1):105-115.
Li Y H,Gao M T,Wu Q J.2014.Crustal thickness map of the Chinese mainland from teleseismic receiver functions.Tectonophysics,611:51-60.
Ligorría J P,Ammon C J.1999.Iterative deconvolution and receiver-function estimation.Bulletin of the Seismological Society of America,89(5):1395-1400.
Liu D L,Chen F J,Guan D F,et al.1996.A study on lithospheric dynamics of the origin and evolution in the Songliao Basin.Scientia Geologica Sinica(in Chinese),31(4):397-408.
Liu H F,Niu F L.2011.Receiver function study of the crustal structure of Northeast China:Seismic evidence for a mantle upwelling beneath the eastern flank of the Songliao Basin and the Changbaishan region.Earthquake Science,24(1):27-33.
Liu Q Y,Kind R,Li S C.1996.Maximal likelihood estimation and nonlinear inversion of the complex receiver function spectrum ratio.Chinese Journal of Geophysics(Acta Geophysica Sinica)(in Chinese),39(4):500-511.
Lu Z X,Xia H K.1993.Geoscience transect from Dong Ujimqinqi,Nei Mongol,to Donggou,Liaoning,China.Chinese Journal of Geophysics(Acta Geophysica Sinica)(in Chinese),36(6):766-772.
Lu Z X,Xia H K,Zhao G M,et al.1993.Synthetic geophysics feature of geoscience transection from Dong Ujimqin Qi,Nei Mongol to Donggou,Liaoning.Seismological Research of Northeast China(in Chinese),9(2):1-12.
Niu F L,Li J.2011.Component azimuths of the CEArray stations estimated from P-wave particle motion.Earthquake Science,24(1):3-13.
Owens T J,Zandt G,Taylor S R.1984.Seismic evidence for an ancient rift beneath the Cumberland Plateau,Tennessee:Adetailed analysis of broadband teleseismic Pwaveforms.Journal of Geophysical Research:Solid Earth,89(B9):7783-7795.
Qiu G G,Fei F G,Fang H,et al.2014.Analysis of magma chamber at the Tianchi volcano area in Changbai mountain.Chinese Journal of Geophysics(in Chinese),57(10):3466-3477,doi:10.6038/cjg20141032.
Saikia S,Chopra S,Baruah S,et al.2017.Shallow sedimentary structure of the Brahmaputra Valley constraint from receiver functions analysis.Pure and Applied Geophysics,174(1):229-247.
Shao J A,Tang K D,Zhan L P,et al.1995.Reconstruction of an ancient continental margin and its implication:New progress on the study of geology of Yanbian region,northeast China.Science in China(Series B)(in Chinese),25(5):548-555.
Tang J,Deng Q F,Zhao G Z,et al.2001.Electric conductivity and magma chamber at the Tianchi volcano area in Changbaishan mountain.Seismology and Geology(in Chinese),23(2):191-200.
Tang J,Zhao G Z,Wang J J,et al.2006.Study of the formation mechanism for volcanism in Northeast China based on deep electric structure.Acta Petrologica Sinica(in Chinese),22(6):1503-1510.
Tao K,Niu F L,Ning J Y,et al.2014.Crustal structure beneath NE China imaged by NECESSArray receiver function data.Earth and Planetary Science Letters,398:48-57.
Wan T F,Zhu H,Zhao L,et al.1996.Formation and evolution of Tancheng-Lujiang Fault Zone:A review.Geoscience(in Chinese),10(2):159-168.
Wang K Y,Liu D,Liu J R,et al.2015.Crustal seismic in the northeast of China.Progress in Geophysics(in Chinese),30(1):61-69.
Wang W,Chen Q F.2017.The crust S-wave velocity structure under the Changbaishan volcano area in northeast China inferred from ambient noise tomography.Chinese Journal of Geophysics(in Chinese),60(8):3080-3095,doi:10.6038/cjg20170816.
Wang X.2016.Seismological study on upper mantle transition zone structure beneath the northwest Pacific subduction region[Ph.D.thesis](in Chinese).Beijing:Institute of Geology and Geophysics,Chinese Academy of Sciences.
Wang X,Chen Q F,Li J,et al.2016.Seismic sensor misorientation measurement using P-wave particle motion:an application to the NECsaids Array.Seismological Research Letters,87(4):901-911.
Watanabe T.1993.Effects of water and melt on seismic velocities and their application to characterization of seismic reflectors.Geophysical Research Letters,20(24):2933-2936.
Wei H H,Liu J L,Meng Q R.2010.Structural and sedimentary evolution of the southern Songliao Basin,northeast China,and implications for hydrocarbon prospectivity.AAPG Bulletin,94(4):533-566.
Wei Z G,Chen L.2012.Regional differences in crustal structure beneath northeastern China and northern North China Craton:constraints from crustal thickness and Vp/Vsratio.Chinese Journal of Geophysics(in Chinese),55(11):3601-3614,doi:10.6038/j.issn.0001-5733.2012.11.009.
Wessel P,Smith W H F.1998.New,improved version of generic mapping tools released.EOS,Transactions American Geophysical Union,79(47):579.
Wu F Y,Ye M,Zhang S H.1995.Geodynamic model of the ManzhouliSuifenhe geoscience transect.Earth Science-Journal of China University of Geosciences(in Chinese),20(5):535-539.
Wu J P,Ming Y H,Zhang H R,et al.2007.Earthquake swarm activity in Changbaishan Tianchi volcano.Chinese Journal of Geophysics(in Chinese),50(4):1089-1096.
Wu J P,Ming Y H,Su W,et al.2009.S-wave velocity structure beneath Changbaishan Tianchi volcano inferred from receiver function.Seismology and Geology(in Chinese),31(4):584-597.
Wu Q J,Tian X B,Zhang N L,et al.2003.Receiver function estimated by maximum entropy deconvolution.Acta Seismologica Sinica(in Chinese),25(4):382-389.
Xiong X S,Gao R,Zhang X Z,et al.2011.The Moho depth of North China and Northeast China revealed by seismic detection.Acta Geoscientica Sinica(in Chinese),32(1):46-56.
Yang B J,Mu S M,Jin X,et al.1996.Synthesized study on the geophysics of Manzhouli-Suifenhe geoscience transect,China.Chinese Journal of Geophysics(Acta Geophysica Sinica)(in Chinese),39(6):772-782.
Yeck W L,Sheehan A F,Schulte-Pelkum V.2013.Sequential H-κstacking to obtain accurate crustal thicknesses beneath sedimentary basins.Bulletin of the Seismological Society of America,103(3):2142-2150.
Zhang G C.2012.The structure of the crust and upper mantle in Northeast China from teleseismic receiver function[Ph.D.thesis](in Chinese).Beijing:Institute of Geophysics,China Earthquake Administration.
Zhang G C,Wu Q J,Pan J T,et al.2013.Study of crustal structure and Poisson ratio of NE China by H-Kstack and CCPstack methods.Chinese Journal of Geophysics(in Chinese),56(12):4084-4094,doi:10.6038/cjg20131213.
Zhang J H,Gao S,Ge W C,et al.2010.Geochronology of the Mesozoic volcanic rocks in the Great Xing′an Range,northeastern China:Implications for subduction-induced delamination.Chemical Geology,276(3-4):144-165.
Zhang K J.1997.North and South China collision along the eastern and southern North China margins.Tectonophysics,270(1-2):145-156.
Zhang R Q,Wu Q J,Sun L,et al.2014.Crustal and lithospheric structure of Northeast China from S-wave receiver functions.Earth and Planetary Science Letters,401:196-205.
Zhang X K,Zhang C K,Zhao J R,et al.2002.Deep seismic sounding investigation into the deep structure of the magma system in Changbaishan Tianchi volcanic region.Acta Seismologica Sinica(in Chinese),24(2):135-143.
Zhang X Z,Yang B J,Wu F Y,et al.2006.The lithosphere structure in the Hingmong-Jihei(Hinggan-Mongolia-Jilin-Heilongjiang)region,northeastern China.Geology in China(in Chinese),33(4):816-823.
Zheng T Y,He Y M,Yang J H,et al.2015.Seismological constraints on the crustal structures generated by continental rejuvenation in northeastern China.Scientific Reports,5:14995.
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.
Zhou J B,Zeng W S,Cao J L,et al.2012.The tectonic framework and evolution of the NE China:from~500Ma to~180 Ma.Journal of Jilin University(Earth Science Edition)(in Chinese),42(5):1298-1316.
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 H X,Tian Y,Liu C,et al.2017.High-resolution crustal structure of Northeast China revealed by teleseismic receiver functions.Chinese Journal of Geophysics(in Chinese),60(5):1676-1689,doi:10.6038/cjg20170506.
Zhu L P,Kanamori H.2000.Moho depth variation in southern California from teleseismic receiver functions.Journal of Geophysical Research:Solid Earth,105(B2):2969-2980.
Zhu L P.2000.Crustal structure across the San Andreas Fault,southern California from teleseismic converted waves.Earth and Planetary Science Letters,179(1):183-190.
Zhu R X,Xu Y G,Zhu G,et al.2012.Destruction of the North China Craton.Science China Earth Science,55(10):1565-1587.
程三友.2006.中国东北地区区域构造特征与中、新生代盆地演化[博士论文].北京:中国地质大学(北京).
邓晋福,莫宣学,赵海玲等.1994.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,8(3):349-356.
邓起东,张培震,冉勇康等.2003.中国活动构造与地震活动.地学前缘,10(S1):66-73.
段永红,张先康,刘志等.2005.长白山-镜泊湖火山区地壳结构接收函数研究.地球物理学报,48(2):352-358.
樊祺诚,隋建立,王团华等.2007.长白山火山活动历史、岩浆演化与喷发机制探讨.高校地质学报,13(2):175-190.
高占永.2015.中国东北地区地壳上地幔结构的接收函数研究[硕士论文].北京:中国地震局地球物理研究所.
国家测震台网数据备份中心.2007-05-23.国家测震台网地震波形数据.中国地震局地球物理研究所,http:∥www.seisdmc.ac.cn.
郭孟习,孙炜,尹国义等.2000.郯庐断裂系的北延及地质-地球物理特征.吉林地质,19(3):35-44.
郭震,唐有彩,陈永顺等.2012.华北克拉通东部地壳和上地幔结构的接收函数研究.地球物理学报,55(11):3591-3600,doi:10.6038/j.issn.0001-5733.2012.11.008.
嵇少丞,王茜,杨文采.2009.华北克拉通泊松比与地壳厚度的关系及其大地构造意义.地质学报,83(3):324-330.
李克,刘俊清,盘晓东等.2009.2000-2007年期间长白山天池火山区地壳变形监测与分析.地震地质,31(4):639-646.
李献甫,陈全茂,张学海等.2002.伊通地堑-走滑断陷盆地的构造特征及演化.石油实验地质,24(1):19-30.
刘德来,陈发景,关德范等.1996.松辽盆地形成、发展与岩石圈动力学.地质科学,31(4):397-408.
刘启元,Kind R,李顺成.1996.接收函数复谱比的最大或然性估计及非线性反演.地球物理学报,39(4):500-511.
卢造勋,夏怀宽.1993.内蒙古东乌珠穆沁旗-辽宁东沟地学断面.地球物理学报,36(6):766-772.
卢造勋,夏怀宽,赵国敏等.1993.内蒙古东乌珠穆沁旗至辽宁东沟地学断面综合地球物理特征.东北地震研究,9(2):1-12.
仇根根,裴发根,方慧等.2014.长白山天池火山岩浆系统分析.地球物理学报,57(10):3466-3477,doi:10.6038/cjg20141032.
邵济安,唐克东,詹立培等.1995.一个古大陆边缘的再造及其大地构造意义---延边地质研究新进展.中国科学(B辑),25(5):548-555.
汤吉,邓前辉,赵国泽等.2001.长白山天池火山区电性结构和岩浆系统.地震地质,23(2):191-200.
汤吉,赵国泽,王继军等.2006.基于地下电性结构探讨中国东北活动火山形成机制.岩石学报,22(6):1503-1510.
万天丰,朱鸿,赵磊等.1996.郯庐断裂带的形成与演化:综述.现代地质,10(2):159-168.
王开燕,刘丹,柳俊茹等.2015.东北地区地壳结构研究.地球物理学进展,30(1):61-69.
王武,陈棋福.2017.长白山火山区地壳S波速度结构的背景噪声成像.地球物理学报,60(8):3080-3095,doi:10.6038/cjg20170816.
王新.2016.西北太平洋俯冲区上地幔过渡带的地震学研究[博士论文].北京:中国科学院地质与地球物理研究所.
危自根,陈凌.2012.东北地区至华北北缘地壳结构的区域差异:地壳厚度与波速比的联合约束.地球物理学报,55(11):3601-3614,doi:10.6038/j.issn.0001-5733.2012.11.009.
吴福元,叶茂,张世红.1995.中国满洲里-绥芬河地学断面域的地球动力学模型.地球科学---中国地质大学学报,20(5):535-539.
吴建平,明跃红,张恒荣等.2007.长白山天池火山区的震群活动研究.地球物理学报,50(4):1089-1096.
吴建平,明跃红,苏伟等.2009.长白山火山区壳幔S波速度结构研究.地震地质,31(4):584-597.
吴庆举,田小波,张乃玲等.2003.计算台站接收函数的最大熵谱反褶积方法.地震学报,25(4):382-389.
熊小松,高锐,张兴洲等.2011.深地震探测揭示的华北及东北地区莫霍面深度.地球学报,32(1):46-56.
杨宝俊,穆石敏,金旭等.1996.中国满洲里-绥芬河地学断面地球物理综合研究.地球物理学报,39(6):772-782.
张广成.2012.用接收函数方法研究中国东北地区地壳上地幔结构[博士论文].北京:中国地震局地球物理研究所.
张广成,吴庆举,潘佳铁等.2013.利用H-K叠加方法和CCP叠加方法研究中国东北地区地壳结构与泊松比.地球物理学报,56(12):4084-4094,doi:10.6038/cjg20131213.
张先康,张成科,赵金仁等.2002.长白山天池火山区岩浆系统深部结构的深地震测深研究.地震学报,24(2):135-143.
张兴洲,杨宝俊,吴福元等.2006.中国兴蒙-吉黑地区岩石圈结构基本特征.中国地质,33(4):816-823.
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.
周建波,曾维顺,曹嘉麟等.2012.中国东北地区的构造格局与演化:从500Ma到180 Ma.吉林大学学报(地球科学版),42(5):1298-1316.
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.
朱洪翔,田有,刘财等.2017.中国东北地区高分辨率地壳结构:远震接收函数.地球物理学报,60(5):1676-1689,doi:10.6038/cjg20170506.
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.
Chen L,Zheng T Y,Xu W W.2006.A thinned lithospheric image of the Tanlu Fault Zone,eastern China:Constructed from wave equation based receiver function migration.Journal of Geophysical Research:Solid Earth,111(B9):B09312,doi:10.1029/2005JB003974.
Chen Y L,Niu F L,Liu R F,et al.2010.Crustal structure beneath China from receiver function analysis.Journal of Geophysical Research:Solid Earth,115(B3):B03307,doi:10.1029/2009JB006386.
Cheng S Y.2006.Regional tectonic characters and Meso-Cenozoic basin evolution in Northeastern China[Ph.D.thesis](in Chinese).Beijing:China University of Geosciences,Beijing.
Data Management Centre of China National Seismic Network.2007-05-23.Waveform data of China National Seismic Network.Institute of Geophysics,China Earthquake Administration,http:∥www.seisdmc.ac.cn.
DeMets C,Gordon R G,Argus D F,et al.1994.Effect of recent revisions to the geomagnetic reversal time scale on estimates of current plate motions.Geophysical Research Letters,21(20):2191-2194.
Deng J F,Mo X X,Zhao H L,et al.1994.Lithosphere root/derooting and activation of the east China continent.Geoscience(in Chinese),8(3):349-356.
Deng Q D,Zhang P Z,Ran Y K,et al.2003.Active tectonics and earthquake activities in China.Earth Science Frontiers(in Chinese),10(S1):66-73.
Duan Y H,Zhang X K,Liu Z,et al.2005.A study on crustal structures of Changbaishan-Jingpohu volcanic area using receiver functions.Chinese Journal of Geophysics(in Chinese),48(2):352-358.
Dueker K G,Sheehan A F.1997.Mantle discontinuity structure from midpoint stacks of converted P to S waves across the Yellowstone hotspot track.Journal of Geophysical Research:Solid Earth,102(B4):8313-8327.
Efron B,Tibshirani R.1986.Bootstrap methods for standard errors,confidence intervals,and other measures of statistical accuracy.Statistical Science,1(1):54-75.
Fan Q C,Sui J L,Wang T H,et al.2007.History of volcanic activity,magma evolution and eruptive mechanisms of the Changbai volcanic province.Geological Journal of China Universities(in Chinese),13(2):175-190.
Gao Z Y.2015.The study of the crustal and upper mantle structure in Northeast China from teleseismic receiver function[Master′s thesis](in Chinese).Beijing:Institute of Geophysics,China Earthquake Administration.
Guo M X,Sun W,Yin G Y,et al.2000.North-extension of the Tanlu fracture and geologic-geophysical characteristics.Jilin Geology(in Chinese),19(3):35-44.
Guo Z,Tang Y C,Chen John,et al.2012.A study on crustal and upper mantle structures in east part of North China Craton using receiver functions.Chinese Journal of Geophysics(in Chinese),55(11):3591-3600,doi:10.6038/j.issn.0001-5733.2012.11.008.
Guo Z,Chen Y J,Ning J Y,et al.2015.High resolution 3-Dcrustal structure beneath NE China from joint inversion of ambient noise and receiver functions using NECESSArray data.Earth and Planetary Science Letters,416:1-11.
Guo Z,Chen Y J,Ning J Y,et al.2016.Seismic evidence of ongoing sublithosphere upper mantle convection for intra-plate volcanism in Northeast China.Earth and Planetary Science Letters,433:31-43.
He C S,Dong S W,Santosh M,et al.2013.Seismic evidence for a geosuture between the Yangtze and Cathaysia Blocks,South China.Scientific Reports,3:2200.
He R Z,Shan 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.
Hetland E A,Wu F T,Song J L.2004.Crustal structure in the Changbaishan volcanic area,China,determined by modeling receiver functions.Tectonophysics,386(3-4):157-175.
Ji S C,Wang X,Yang W C.2009.Correlation between crustal thickness and Poisson′s ratio in the North China Craton and its implication for lithospheric thinning.Acta Geologica Sinica(in Chinese),83(3):324-330.
Kennett B L N,Engdahl E R.1991.Traveltimes for global earthquake location and phase identification.Geophysical Journal International,105(2):429-465.
Kind R,Yuan X H,Kumar P.2012.Seismic receiver functions and the lithosphere-asthenosphere boundary.Tectonophysics,536-537:25-43.
Kyong-Song R,Hammond J O S,Chol-Nam K,et al.2016.Evidence for partial melt in the crust beneath Mt.Paektu(Changbaishan),Democratic People′s Republic of Korea and China.Science Advances,2(4):e1501513.
Langston C A.1979.Structure under Mount Rainier,Washington,inferred from teleseismic body waves.Journal of Geophysical Research:Solid Earth,84(B9):4749-4762.
Li K,Liu J Q,Pan X D,et al.2009.Crust deformation monitoring and research in Tianchi volcanic area,Changbai mountains from 2000-2007.Seismology and Geology(in Chinese),31(4):639-646.
Li X F,Chen Q M,Zhang X H,et al.2002.The Yitong grabenthe structural features and evolution of a strike-slip fault basin.Petroleum Geology&Experiment(in Chinese),24(1):19-30.
Li Y H,Wu Q J,Pan J T,et al.2012.S-wave velocity structure of northeastern China from joint inversion of Rayleigh wave phase and group velocities.Geophysical Journal International,190(1):105-115.
Li Y H,Gao M T,Wu Q J.2014.Crustal thickness map of the Chinese mainland from teleseismic receiver functions.Tectonophysics,611:51-60.
Ligorría J P,Ammon C J.1999.Iterative deconvolution and receiver-function estimation.Bulletin of the Seismological Society of America,89(5):1395-1400.
Liu D L,Chen F J,Guan D F,et al.1996.A study on lithospheric dynamics of the origin and evolution in the Songliao Basin.Scientia Geologica Sinica(in Chinese),31(4):397-408.
Liu H F,Niu F L.2011.Receiver function study of the crustal structure of Northeast China:Seismic evidence for a mantle upwelling beneath the eastern flank of the Songliao Basin and the Changbaishan region.Earthquake Science,24(1):27-33.
Liu Q Y,Kind R,Li S C.1996.Maximal likelihood estimation and nonlinear inversion of the complex receiver function spectrum ratio.Chinese Journal of Geophysics(Acta Geophysica Sinica)(in Chinese),39(4):500-511.
Lu Z X,Xia H K.1993.Geoscience transect from Dong Ujimqinqi,Nei Mongol,to Donggou,Liaoning,China.Chinese Journal of Geophysics(Acta Geophysica Sinica)(in Chinese),36(6):766-772.
Lu Z X,Xia H K,Zhao G M,et al.1993.Synthetic geophysics feature of geoscience transection from Dong Ujimqin Qi,Nei Mongol to Donggou,Liaoning.Seismological Research of Northeast China(in Chinese),9(2):1-12.
Niu F L,Li J.2011.Component azimuths of the CEArray stations estimated from P-wave particle motion.Earthquake Science,24(1):3-13.
Owens T J,Zandt G,Taylor S R.1984.Seismic evidence for an ancient rift beneath the Cumberland Plateau,Tennessee:Adetailed analysis of broadband teleseismic Pwaveforms.Journal of Geophysical Research:Solid Earth,89(B9):7783-7795.
Qiu G G,Fei F G,Fang H,et al.2014.Analysis of magma chamber at the Tianchi volcano area in Changbai mountain.Chinese Journal of Geophysics(in Chinese),57(10):3466-3477,doi:10.6038/cjg20141032.
Saikia S,Chopra S,Baruah S,et al.2017.Shallow sedimentary structure of the Brahmaputra Valley constraint from receiver functions analysis.Pure and Applied Geophysics,174(1):229-247.
Shao J A,Tang K D,Zhan L P,et al.1995.Reconstruction of an ancient continental margin and its implication:New progress on the study of geology of Yanbian region,northeast China.Science in China(Series B)(in Chinese),25(5):548-555.
Tang J,Deng Q F,Zhao G Z,et al.2001.Electric conductivity and magma chamber at the Tianchi volcano area in Changbaishan mountain.Seismology and Geology(in Chinese),23(2):191-200.
Tang J,Zhao G Z,Wang J J,et al.2006.Study of the formation mechanism for volcanism in Northeast China based on deep electric structure.Acta Petrologica Sinica(in Chinese),22(6):1503-1510.
Tao K,Niu F L,Ning J Y,et al.2014.Crustal structure beneath NE China imaged by NECESSArray receiver function data.Earth and Planetary Science Letters,398:48-57.
Wan T F,Zhu H,Zhao L,et al.1996.Formation and evolution of Tancheng-Lujiang Fault Zone:A review.Geoscience(in Chinese),10(2):159-168.
Wang K Y,Liu D,Liu J R,et al.2015.Crustal seismic in the northeast of China.Progress in Geophysics(in Chinese),30(1):61-69.
Wang W,Chen Q F.2017.The crust S-wave velocity structure under the Changbaishan volcano area in northeast China inferred from ambient noise tomography.Chinese Journal of Geophysics(in Chinese),60(8):3080-3095,doi:10.6038/cjg20170816.
Wang X.2016.Seismological study on upper mantle transition zone structure beneath the northwest Pacific subduction region[Ph.D.thesis](in Chinese).Beijing:Institute of Geology and Geophysics,Chinese Academy of Sciences.
Wang X,Chen Q F,Li J,et al.2016.Seismic sensor misorientation measurement using P-wave particle motion:an application to the NECsaids Array.Seismological Research Letters,87(4):901-911.
Watanabe T.1993.Effects of water and melt on seismic velocities and their application to characterization of seismic reflectors.Geophysical Research Letters,20(24):2933-2936.
Wei H H,Liu J L,Meng Q R.2010.Structural and sedimentary evolution of the southern Songliao Basin,northeast China,and implications for hydrocarbon prospectivity.AAPG Bulletin,94(4):533-566.
Wei Z G,Chen L.2012.Regional differences in crustal structure beneath northeastern China and northern North China Craton:constraints from crustal thickness and Vp/Vsratio.Chinese Journal of Geophysics(in Chinese),55(11):3601-3614,doi:10.6038/j.issn.0001-5733.2012.11.009.
Wessel P,Smith W H F.1998.New,improved version of generic mapping tools released.EOS,Transactions American Geophysical Union,79(47):579.
Wu F Y,Ye M,Zhang S H.1995.Geodynamic model of the ManzhouliSuifenhe geoscience transect.Earth Science-Journal of China University of Geosciences(in Chinese),20(5):535-539.
Wu J P,Ming Y H,Zhang H R,et al.2007.Earthquake swarm activity in Changbaishan Tianchi volcano.Chinese Journal of Geophysics(in Chinese),50(4):1089-1096.
Wu J P,Ming Y H,Su W,et al.2009.S-wave velocity structure beneath Changbaishan Tianchi volcano inferred from receiver function.Seismology and Geology(in Chinese),31(4):584-597.
Wu Q J,Tian X B,Zhang N L,et al.2003.Receiver function estimated by maximum entropy deconvolution.Acta Seismologica Sinica(in Chinese),25(4):382-389.
Xiong X S,Gao R,Zhang X Z,et al.2011.The Moho depth of North China and Northeast China revealed by seismic detection.Acta Geoscientica Sinica(in Chinese),32(1):46-56.
Yang B J,Mu S M,Jin X,et al.1996.Synthesized study on the geophysics of Manzhouli-Suifenhe geoscience transect,China.Chinese Journal of Geophysics(Acta Geophysica Sinica)(in Chinese),39(6):772-782.
Yeck W L,Sheehan A F,Schulte-Pelkum V.2013.Sequential H-κstacking to obtain accurate crustal thicknesses beneath sedimentary basins.Bulletin of the Seismological Society of America,103(3):2142-2150.
Zhang G C.2012.The structure of the crust and upper mantle in Northeast China from teleseismic receiver function[Ph.D.thesis](in Chinese).Beijing:Institute of Geophysics,China Earthquake Administration.
Zhang G C,Wu Q J,Pan J T,et al.2013.Study of crustal structure and Poisson ratio of NE China by H-Kstack and CCPstack methods.Chinese Journal of Geophysics(in Chinese),56(12):4084-4094,doi:10.6038/cjg20131213.
Zhang J H,Gao S,Ge W C,et al.2010.Geochronology of the Mesozoic volcanic rocks in the Great Xing′an Range,northeastern China:Implications for subduction-induced delamination.Chemical Geology,276(3-4):144-165.
Zhang K J.1997.North and South China collision along the eastern and southern North China margins.Tectonophysics,270(1-2):145-156.
Zhang R Q,Wu Q J,Sun L,et al.2014.Crustal and lithospheric structure of Northeast China from S-wave receiver functions.Earth and Planetary Science Letters,401:196-205.
Zhang X K,Zhang C K,Zhao J R,et al.2002.Deep seismic sounding investigation into the deep structure of the magma system in Changbaishan Tianchi volcanic region.Acta Seismologica Sinica(in Chinese),24(2):135-143.
Zhang X Z,Yang B J,Wu F Y,et al.2006.The lithosphere structure in the Hingmong-Jihei(Hinggan-Mongolia-Jilin-Heilongjiang)region,northeastern China.Geology in China(in Chinese),33(4):816-823.
Zheng T Y,He Y M,Yang J H,et al.2015.Seismological constraints on the crustal structures generated by continental rejuvenation in northeastern China.Scientific Reports,5:14995.
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.
Zhou J B,Zeng W S,Cao J L,et al.2012.The tectonic framework and evolution of the NE China:from~500Ma to~180 Ma.Journal of Jilin University(Earth Science Edition)(in Chinese),42(5):1298-1316.
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 H X,Tian Y,Liu C,et al.2017.High-resolution crustal structure of Northeast China revealed by teleseismic receiver functions.Chinese Journal of Geophysics(in Chinese),60(5):1676-1689,doi:10.6038/cjg20170506.
Zhu L P,Kanamori H.2000.Moho depth variation in southern California from teleseismic receiver functions.Journal of Geophysical Research:Solid Earth,105(B2):2969-2980.
Zhu L P.2000.Crustal structure across the San Andreas Fault,southern California from teleseismic converted waves.Earth and Planetary Science Letters,179(1):183-190.
Zhu R X,Xu Y G,Zhu G,et al.2012.Destruction of the North China Craton.Science China Earth Science,55(10):1565-1587.
程三友.2006.中国东北地区区域构造特征与中、新生代盆地演化[博士论文].北京:中国地质大学(北京).
邓晋福,莫宣学,赵海玲等.1994.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,8(3):349-356.
邓起东,张培震,冉勇康等.2003.中国活动构造与地震活动.地学前缘,10(S1):66-73.
段永红,张先康,刘志等.2005.长白山-镜泊湖火山区地壳结构接收函数研究.地球物理学报,48(2):352-358.
樊祺诚,隋建立,王团华等.2007.长白山火山活动历史、岩浆演化与喷发机制探讨.高校地质学报,13(2):175-190.
高占永.2015.中国东北地区地壳上地幔结构的接收函数研究[硕士论文].北京:中国地震局地球物理研究所.
国家测震台网数据备份中心.2007-05-23.国家测震台网地震波形数据.中国地震局地球物理研究所,http:∥www.seisdmc.ac.cn.
郭孟习,孙炜,尹国义等.2000.郯庐断裂系的北延及地质-地球物理特征.吉林地质,19(3):35-44.
郭震,唐有彩,陈永顺等.2012.华北克拉通东部地壳和上地幔结构的接收函数研究.地球物理学报,55(11):3591-3600,doi:10.6038/j.issn.0001-5733.2012.11.008.
嵇少丞,王茜,杨文采.2009.华北克拉通泊松比与地壳厚度的关系及其大地构造意义.地质学报,83(3):324-330.
李克,刘俊清,盘晓东等.2009.2000-2007年期间长白山天池火山区地壳变形监测与分析.地震地质,31(4):639-646.
李献甫,陈全茂,张学海等.2002.伊通地堑-走滑断陷盆地的构造特征及演化.石油实验地质,24(1):19-30.
刘德来,陈发景,关德范等.1996.松辽盆地形成、发展与岩石圈动力学.地质科学,31(4):397-408.
刘启元,Kind R,李顺成.1996.接收函数复谱比的最大或然性估计及非线性反演.地球物理学报,39(4):500-511.
卢造勋,夏怀宽.1993.内蒙古东乌珠穆沁旗-辽宁东沟地学断面.地球物理学报,36(6):766-772.
卢造勋,夏怀宽,赵国敏等.1993.内蒙古东乌珠穆沁旗至辽宁东沟地学断面综合地球物理特征.东北地震研究,9(2):1-12.
仇根根,裴发根,方慧等.2014.长白山天池火山岩浆系统分析.地球物理学报,57(10):3466-3477,doi:10.6038/cjg20141032.
邵济安,唐克东,詹立培等.1995.一个古大陆边缘的再造及其大地构造意义---延边地质研究新进展.中国科学(B辑),25(5):548-555.
汤吉,邓前辉,赵国泽等.2001.长白山天池火山区电性结构和岩浆系统.地震地质,23(2):191-200.
汤吉,赵国泽,王继军等.2006.基于地下电性结构探讨中国东北活动火山形成机制.岩石学报,22(6):1503-1510.
万天丰,朱鸿,赵磊等.1996.郯庐断裂带的形成与演化:综述.现代地质,10(2):159-168.
王开燕,刘丹,柳俊茹等.2015.东北地区地壳结构研究.地球物理学进展,30(1):61-69.
王武,陈棋福.2017.长白山火山区地壳S波速度结构的背景噪声成像.地球物理学报,60(8):3080-3095,doi:10.6038/cjg20170816.
王新.2016.西北太平洋俯冲区上地幔过渡带的地震学研究[博士论文].北京:中国科学院地质与地球物理研究所.
危自根,陈凌.2012.东北地区至华北北缘地壳结构的区域差异:地壳厚度与波速比的联合约束.地球物理学报,55(11):3601-3614,doi:10.6038/j.issn.0001-5733.2012.11.009.
吴福元,叶茂,张世红.1995.中国满洲里-绥芬河地学断面域的地球动力学模型.地球科学---中国地质大学学报,20(5):535-539.
吴建平,明跃红,张恒荣等.2007.长白山天池火山区的震群活动研究.地球物理学报,50(4):1089-1096.
吴建平,明跃红,苏伟等.2009.长白山火山区壳幔S波速度结构研究.地震地质,31(4):584-597.
吴庆举,田小波,张乃玲等.2003.计算台站接收函数的最大熵谱反褶积方法.地震学报,25(4):382-389.
熊小松,高锐,张兴洲等.2011.深地震探测揭示的华北及东北地区莫霍面深度.地球学报,32(1):46-56.
杨宝俊,穆石敏,金旭等.1996.中国满洲里-绥芬河地学断面地球物理综合研究.地球物理学报,39(6):772-782.
张广成.2012.用接收函数方法研究中国东北地区地壳上地幔结构[博士论文].北京:中国地震局地球物理研究所.
张广成,吴庆举,潘佳铁等.2013.利用H-K叠加方法和CCP叠加方法研究中国东北地区地壳结构与泊松比.地球物理学报,56(12):4084-4094,doi:10.6038/cjg20131213.
张先康,张成科,赵金仁等.2002.长白山天池火山区岩浆系统深部结构的深地震测深研究.地震学报,24(2):135-143.
张兴洲,杨宝俊,吴福元等.2006.中国兴蒙-吉黑地区岩石圈结构基本特征.中国地质,33(4):816-823.
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.
周建波,曾维顺,曹嘉麟等.2012.中国东北地区的构造格局与演化:从500Ma到180 Ma.吉林大学学报(地球科学版),42(5):1298-1316.
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.
朱洪翔,田有,刘财等.2017.中国东北地区高分辨率地壳结构:远震接收函数.地球物理学报,60(5):1676-1689,doi:10.6038/cjg20170506.
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.
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