引文
[1]耿树方,刘平,王振洋,等.亚洲地球动力系统的演进与东亚矿产资源效应[J].中国地质,2010,37(4):866-880.
[2]Zhao D,Hasegawa A,Horiuchi S.Tomographic imaging of P and Swave velocity structure beneath northeastern Japan[J].J.Geophys.Res.,1992,97:19909-19928.
[3]Zhao D,Hasegawa A,Kanamori H.Deep structure of Japan subduc-tion zone as derived from local,regional,and teleseismic events[J].J.Geophys.Res.,1994,99(B11):22313-22329.
[4]Um J,Thurber C H.A fast algorithm for two-point seismic ray trac-ing[J].Bull.Seismol.Soc.Am.,1987,77:972-986.
[5]Paige C C,Saunders M A.LSQR:An algorithm for sparse linearequations and sparse least squares[J].Assoc.Comput.Mach.Trans.Math.Soferware,1982,8:43-71.
[6]Humphreys E R,Clayton R W.Adaptation of back projection to-mography to seismic travel time problems[J].J.Geophys.Res.,1988,93:1073-1085.
[7]Liang C,Song X,Huang J.Tomographic inversion of Pn travel times inChina[J].J.Geophys.Res.,2004,109,B11304,doi:10.1029/2003JB002789.
[8]Huang J L,Zhao D.Hight-resolution mantle tomography of Chinaand Surrounding regions[J].J.Geophysical.R.,2006,111,B09305.
[9]Zhao D,Lei J.Seismic ray path variations in a 3D global velocitymodel[J].Phys.Earth Planet Inter.,2004,141:153-166.
[10]周新华,陈义贤,张国辉,等.中生代火山岩源区特征的多元同位素制约——以华北北缘为例[J].科学通报,1998,43(23):2483-2488.
[11]周新华,张国辉,杨进辉,等.华北克拉通北缘晚中生代火山岩Sr-Nd-Pb同位素填图及其构造意义[J].地球化学,2001,30(1):10-23.
[12]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[J].地学前缘,2006,13(2):50-64.
[13]陈义贤,陈文寄.辽西及邻区中生代火山岩-年代学、地球化学和构造背景[M].北京:地震出版社,1997:12-79.
[14]Huang Z,Li H,Zheng Y,et al.The lithosphere of North China Cra-ton from surface wave tomography[J].Earth Planet.Sci.Lett.,2009,288(1/2):164-173.
[15]刘国栋,顾群,史书林,等.京津唐渤和周围地区地壳上地幔电性结构及其与地震活动关系[J].地球物理学报,1983,26(2):186-197.
[16]朱介寿,曹家敏,蔡学林,等.东亚及西太平洋边缘海高分辨率面波层析成像[J].地球物理学报,2002,45(5):646-664.
[17]Pei S,Chen Y.Tomgraphic structure of East Asia:I.No fast(slab)anomalies beneath 660 km discontinuity[J].Earthq.Sci.,2010,23:597-611.
[18]Pei S,Zhao J,Sun Y,et al.Upper mantle seismic velocities andanisotropy in China determined through Pn and Sn tomography[J].J.Geophys.Res.,2007,112,B05312.
[19]Huang Z,Wang L,Zhao D,et al.Upper mantle structure and dynam-ics beneath Southeast China[J].Phys.Earth Planet.Inter.,2010,182:161-169.
[20]Northrup C,Royden L,Burchfiel B.Motion of the Pacific plate rela-tive to Eurasia and its potential relation to Cenozoic extension alongthe eastern margin of Eurasia[J].Geology,1995,23(8):719-722.
[21]廖其林.台湾海峡海洋综合地球物理研究最新成果评述[J].国际地震动态,1992,12:1-4.
[22]Xu X,Ma X.Geodynamics of the Shanxi Rift system,China[J].Tectonophysics,1992,208:325-340.
[23]Deng J,Zhao H,Luo Z et al.Mantle plumes and lithosphere motionin east Asia[C]//Flower F J M,Chung S L,Lo C H,et al.MantleDynamics and Plate Interactions In East Asia,Geodynamics Series.American Geophysical Union,Washington,DC,1998:59-66.
[24]刘翠,邓晋福,苏尚国,等.华北地区燕山期岩浆活动热供给的初步数值模拟[J].地学前缘,2006,1(2):158-164.
[25]Liu M,Cui X,Liu F.Cenozoic rifting and volcanism in eastern Chi-na:a mantle dynamic link to the Indo-Asian collision?[J].Tectono-physics,2004,33:29-42.
[26]李延兴,张静华,李智,等.太平洋板块俯冲对中国大陆的影响[J].测绘学报,2006,35(2):99-105.
[27]Zhang Y S.Three-dimensional upper mantle structure beneath EastAsia and its tectonic implications[C]//Flower M F J,Chung S L,LoC H,et al.Mantle Dynamics and Plate Interactions in East Asia.Geodynamics Series.American Geophysical Union,Washington,DC,1998:11-23.