引文
[1]Liu D Y,Nutman A P,Compston W,et al.Remnants of≥3800Ma crust in the Chinese part of the Sino-Korean craton.Geology,1992,20(4):339-342.
[2]Ren J Y,Tamakib K,Li S,et al.Late Mesozoic andCenozoic rifting and its dynamic setting in Eastern China andadjacent areas.Tectonophysics,2002,344(3-4):175-205.
[3]Xu Y G,Chuang S L,Ma J L,et al.Contrasting Cenozoiclithospheric evolution and architecture in the western andeastern Sino-Korean craton:Constraints from geochemistryof basalts and mantle xenoliths.The Journal of Geology,2004,112(5):593-605.
[4]Gao S,Rudnick R L,Yuan H L,et al.Recycling lowercontinental crust in the North China craton.Nature,2004,432(7019):892-897.
[5]周新华.中国东部中、新生代岩石圈转型与减薄研究若干问题.地学前缘,2006,13(2).Zhou X H.Major transformation of subcontinentallithosphere beneath eastern China in the Cenozoic-Mesozoic:review and prospect.Earth Science Frontiers(in Chinese),2006,13(2):50-64.
[6]Chen L,Tao Wang,Zhao L,et al.Distinct lateral variationof lithospheric thickness in the northeastern North ChinaCraton.Earth and Planetary Science Letters,2008,267(1-2):56-68.
[7]吴福元,葛文春,孙德有等.中国东部岩石圈减薄研究中的几个问题.地学前缘,2003,10(3):51-60.Wu F Y,Ge W C,Sun D Y,et al.Discussions on thelithospheric thinning in eastern China.Earth ScienceFrontiers(in Chinese),2003,10(3):51-60.
[8]Menzies M A,Fan W M,Zhang M.Palaeozoic and Cenozoiclithoprobe and the loss of>120km of Archean lithosphere,Sino-Korean craon,China.//Magmatic processes and platetectonics.1993:10.
[9]吴福元,孙德有.中国东部中生代岩浆作用与岩石圈减薄.长春科技大学学报,1999,29(4):313-318.Wu F Y,Sun D Y.The Mesozoic magmatism andlithospheric thinning in eastern China.Journal ofChangchun University of Science and Technology(inChinese),1999,29(4):313-318.
[10]Xu Y G,Chung S L,Ma J L,et al.Contrasting Cenozoiclithospheric evolution and architecture in the western andeastern Sino-Korean Craton:constraints from geochemistryof basalts and mantle xenoliths.The Journal of Geology,2004,112(5):593-605.
[11]Chen L,Zheng T Y,Xu W W.A thinned lithospheric imageof the Tanlu Fault Zone,eastern China:Constructed fromwave equation based receiver function migration.Journal ofGeophysical Research,2006,111:B09312,doi:10.1029/2005JB003974.
[12]Langston C A.Structure under mount rainier,Washington,inferred from teleseismic body waves.Journal of GeophysicalResearch,1979,84(Nb9):4749-4762.
[13]Yuan X H,Kind R,Li X Q,et al.The S receiver functions:synthetics and data example.Geophysical Journal International,2006,165(2):555-564.
[14]Dueker K G,Sheehan A F.Mantle discontinuity structurefrom midpoint stacks of converted P to S waves across theYellowstone hotspot track.Journal of Geophysical Research,1997,102(B4):8313-8327.
[15]李理,钟大赉,时秀朋.鲁西隆起和济阳凹陷新生代隆坳耦合关系.地质学报,2007,81(9):1215-1228.Li L,Zhong D L,Shi X P.Cenozoic uplifting/subsidencecoupling between the West Shandong Rise and the JiyangDepression,Northern China.Acta Geologica Sinica(inChinese),2007,81(9):1215-1228.
[16]张锡明,张岳桥,季玮.山东鲁西地块断裂构造分布型式与中生代沉积-岩浆-构造演化序列.地质力学学报,2007,13(2):163-172.Zhang X M,Zhang Y Q,Ji W.Fault distribution patterns ofthe Luxi block,Shandong,and Mesozoic sedimentary-magmatic-structural evolution sequence.Journal of Geomechanics(in Chinese),2007,13(2):163-172.
[17]邱瑞照,邓晋福,周肃等.华北地区岩石圈类型:地质与地球物理证据.中国科学D辑地球科学,2004,34(8):698-711.Qiu R Z,Deng J F,Zhou S,et al.Lithosphere types inNorth China-Evidences from geology and geophysics.Sciencein China(Ser.D),2005,48(11):1809-1827.
[18]牛树银,胡华斌,毛景文等.鲁西地区地质构造特征及其形成机制.中国地质,2004,31(1):34-39.Niu S Y,Hu H B,Mao J W,et al.Structure in westernShandong and its genetic mechanism.Acta Geologica Sinica(in Chinese),2004,31(1):34-39.
[19]许志琴,张泽明,刘福来等.苏鲁高压-超高压变质带的折返构造及折返机制.地质学报,2003,77(4):433-450.Xu Z Q,Zhang Z M,Liu F L,et al.Exhumation structureand mechanism of the Sulu ultrahigh-pressure metamorphicbelt,Central China.Acta Geologica Sinica(in Chinese),2003,77(4):433-450.
[20]杨文采,程振炎,陈国九等.苏鲁超高压变质带北部地球物理调查(I)——深反射地震.地球物理学报,1999,42(1):41-52.Yang W C,Cheng Z Y,Chen G J,et al.Ceophysicalinvestigations in northern Sulu UHPM belt,part I:deepseismic reeflection.Chinese J.Geophys.(in Chinese),1999,42(1):41-52.
[21]Ligorría J P,Ammon C J.Iterative deconvolution andreceiver-function estimation.Bulletin of the SeismologicalSociety of America,1999,89(5):1395-1400.
[22]Kennett B L N.The removal of free surface interactions fromthree-component seismograms.Geophysical Journal International,1991,104(1):153-154.
[23]Wilson D,Aster R.Seismic imaging of the crust and uppermantle using regularized joint receiver functions,frequency-wave number filtering,and multimode Kirchhoff migration.Journal of Geophysical Research,2005,110:B05305,doi:10.1029/2004JB003430.
[24]Shapiro N M,Ritzwoller M H.Monte-Carlo inversion for aglobal shear-velocity model of the crust and upper mantle.Geophysical Journal International,2002,151(1):88-105.
[25]Zhao L,Zheng T Y,Xu W W.Modeling the Jiyangdepression,northern China,using a wave-field extrapolationfinite-difference method and waveform inversion.Bulletin ofthe Seismological Society of America,2004,94(3):988-1001.
[26]朱光,牛漫兰,宋传中等.郯庐断裂带新生代的上地幔剪切作用与火山活动.安徽地质,2001,11(2):106-112.Zhu G,Niu M L,Song Z Z,et al.Upper mantle shearingand volcanic activities along the Tan-lu fault zone inCenozoic.Geology of Anhui(in Chinese),2001,11(2):106-112.
[27]Zhu L P,Kanamori H.Moho depth variation in southernCalifornia from teleseismic receiver functions.Journal ofGeophysical Research,2000,105(B2):2969-2980.
[28]Owens T J,Zandt G.Implications of crustal propertyvariations for models of Tibetan plateau evolution.Nature,1997,387(6628):37-43.
[29]Zandt G,Ammon C J.Continental crust compositionconstrained by measurements of crustal Poisson′s ratio.Nature,1995,374(6518):152-154.
[30]许卫卫,郑天愉.渤海湾盆地北西盆山边界地区泊松比分布.地球物理学报,2005,48(5):1077-1084.Xu W W,Zheng T Y.Distribution of Poisson's ratios in thenorthwestern basin-mountain boundary of the Bohai BayBasin.Chinese Journal of Geophysics(in Chinese),2005,48(5):1077-1084.