用接收函数方法研究华北地区地壳方位各向异性特征
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- 论文作者：杨妍 ; 姚华建 ; 张萍
- 年：2016
- 作者机构：中国科学技术大学;
- 会议召开时间：2016-10-15
- 会议录名称：2016中国地球科学联合学术年会论文集（八）——专题18：地球深内部主要圈层结构、专题19：核幔边界、地核结构及其动力学、专题20：岩石圈结构与大陆动力学
- 语种：中文
- 分类号：P315.2
- 学会代码：ZGDW
- 会议名称：2016中国地球科学联合学术年会
- 会议地点：中国北京
- 主办单位：中国地球物理学会、中国地震学会、全国岩石学与地球动力学研讨会组委会、中国地质学会构造地质学与地球动力学专业委员会、中国地质学会区域地质与成矿专业委员会
- 学会名称：中国地球物理学会
- 页数：2
- 文件大小：1118k
- 原文格式：D
- 会议级别：全国
摘要
<正>自20世纪60年代Hess在太平洋地区发现Pn波各向异性以来,越来越多的研究发现了地震各向异性现象普遍存在于地球内部。地震波各向异性包含着地球内部的构造变形、动力学过程等方面的信息,研究地壳各向异性特征是提供较高分辨率的区域应力环境和应变状态信息的有效方法之一。华北克拉通的岩石圈演化是现在研究的一个热点问题,研究华北地区的各向异性特征有助于我们对华北地区的深部动力学过程和板块内部应力应变状态之间的关系的深入了解,进而探讨华北克拉通破坏的可
引文
[1]常利军,王椿镛,丁志峰.华北上地幔各向异性研究[J].地球物理学报,2012,03:886-896.
[2]赖院根.流动宽频带地震台阵:首都圈横波分裂与地壳应力场[D].中国地震局地质研究所,2004.
[3]吴晶.地壳介质各向异性区域性特征研究[D].中国地震局地球物理研究所,2007.
[4]吴庆举.宽频带远震体波波形反演方法与青藏高原岩石圈速度结构研究[D].中国地震局地球物理研究所,1996.
[5]武岩.利用接收函数方法研究华北克拉通地壳上地幔结构[D].中国地震局地球物理研究所,2011.
[6]朱日祥,徐义刚,朱光,张宏福,夏群科,郑天愉.华北克拉通破坏[J].中国科学:地球科学,2012,08:1135-1159.
[7]Ammon C J.The isolation of receiver effects from teleseismic P waveforms[J].Bulletin of the seismological Society of America,1991,81(6):2504-2510.
[8]Bowman J R,Ando M.Shear-wave splitting in the upper-mantle wedge above the Tonga subduc-tion zone[J].Geophysical Journal International,1987,88(1):25-41.
[9]Crampin S,Chastin S.A review of shear wave splitting in the crack-critical crust[J].Geophysical Journal International,2003,155(1):221-240.
[10]Crampin S,Lovell J H.A decade of shear-wave splitting in the Earth's crust:what does it mean?what use can we make of it?and what should we do next?[J].Geophysical Journal International,1991,107(3):387-407.
[11]Crampin S.Effective anisotropic elastic constants for wave propagation through cracked sol-ids[J].Geophysical Journal International,1984,76(1):135-145.
[12]Feng J.Distinct variation of depth-dependent azimuthal anisotropy in north china craton re-vealed by ambient noise tomography.In preparation
[13]Frederiksen A W,Bostock M G.Modelling teleseismic waves in dipping anisotropic structures[J].Geophysical Journal International,2000,141(2):401-412
[14]Gao Y,Wu J,Fukao Y,et al.Shear wave splitting in the crust in North China:stress,faults and tectonic implications[J].Geophysical Journal International,2011,187(2):642-654.
[15]Helmberger D,Wiggins R A.Upper mantle structure of midwestern United States[J].Journal of Geophysical Research,1971,76(14):3229-3245.
[16]Hu J,Yang H,Li G,et al.A review on the analysis of the crustal and upper mantle structure using receiver functions[J].Journal of Asian Earth Sciences,2015,111:589-603.
[17]Iidaka T,Niu F.Mantle and crust anisotropy in the eastern China region inferred from wave-form splitting of SKS and Pp Sms[J].Earth,planets and space,2001,53(3):159-168.
[18]Kaneshima S,Ando M.An analysis of split shear waves observed above crustal and uppermost mantle earthquakes beneath Shikoku,Japan:Implications in effective depth extent of seismic ani-sotropy[J].Journal of Geophysical Research:Solid Earth,1989,94(B10):14077-14092.
[19]Langston C A.Structure under Mount Rainier,Washington,inferred from teleseismic body waves[J].Journal of Geophysical Research:Solid Earth,1979,84(B9):4749-4762.
[20]Liu H,Niu F.Estimating crustal seismic anisotropy with a joint analysis of radial and transverse receiver function data[J].Geophysical Journal International,2012,188(1):144-164.
[21]Mc Namara D E,Owens T J.Azimuthal shear wave velocity anisotropy in the Basin and Range province using Moho Ps converted phases[J].Journal of Geophysical Research:Solid Earth,1993,98(B7):12003-12017.
[22]Nagaya M,Oda H,Akazawa H,et al.Receiver functions of seismic waves in layered anisotropic media:Application to the estimate of seismic anisotropy[J].Bulletin of the Seismological Society of America,2008,98(6):2990-3006.
[23]Nicolas A,Christensen N I.Formation of Anisotropy in Upper Mantle Peridotites‐A Review[J].Composition,structure and dynamics of the lithosphere-asthenosphere system,1987:111-123.
[24]Silver P G,Chan W W.Shear wave splitting and subcontinental mantle deformation[J].Journal of Geophysical Research:Solid Earth,1991,96(B10):16429-16454.
[25]Silver P G.Seismic anisotropy beneath the continents:probing the depths of geology[J].Annual review of earth and planetary sciences,1996,24:385-432.
[2]赖院根.流动宽频带地震台阵:首都圈横波分裂与地壳应力场[D].中国地震局地质研究所,2004.
[3]吴晶.地壳介质各向异性区域性特征研究[D].中国地震局地球物理研究所,2007.
[4]吴庆举.宽频带远震体波波形反演方法与青藏高原岩石圈速度结构研究[D].中国地震局地球物理研究所,1996.
[5]武岩.利用接收函数方法研究华北克拉通地壳上地幔结构[D].中国地震局地球物理研究所,2011.
[6]朱日祥,徐义刚,朱光,张宏福,夏群科,郑天愉.华北克拉通破坏[J].中国科学:地球科学,2012,08:1135-1159.
[7]Ammon C J.The isolation of receiver effects from teleseismic P waveforms[J].Bulletin of the seismological Society of America,1991,81(6):2504-2510.
[8]Bowman J R,Ando M.Shear-wave splitting in the upper-mantle wedge above the Tonga subduc-tion zone[J].Geophysical Journal International,1987,88(1):25-41.
[9]Crampin S,Chastin S.A review of shear wave splitting in the crack-critical crust[J].Geophysical Journal International,2003,155(1):221-240.
[10]Crampin S,Lovell J H.A decade of shear-wave splitting in the Earth's crust:what does it mean?what use can we make of it?and what should we do next?[J].Geophysical Journal International,1991,107(3):387-407.
[11]Crampin S.Effective anisotropic elastic constants for wave propagation through cracked sol-ids[J].Geophysical Journal International,1984,76(1):135-145.
[12]Feng J.Distinct variation of depth-dependent azimuthal anisotropy in north china craton re-vealed by ambient noise tomography.In preparation
[13]Frederiksen A W,Bostock M G.Modelling teleseismic waves in dipping anisotropic structures[J].Geophysical Journal International,2000,141(2):401-412
[14]Gao Y,Wu J,Fukao Y,et al.Shear wave splitting in the crust in North China:stress,faults and tectonic implications[J].Geophysical Journal International,2011,187(2):642-654.
[15]Helmberger D,Wiggins R A.Upper mantle structure of midwestern United States[J].Journal of Geophysical Research,1971,76(14):3229-3245.
[16]Hu J,Yang H,Li G,et al.A review on the analysis of the crustal and upper mantle structure using receiver functions[J].Journal of Asian Earth Sciences,2015,111:589-603.
[17]Iidaka T,Niu F.Mantle and crust anisotropy in the eastern China region inferred from wave-form splitting of SKS and Pp Sms[J].Earth,planets and space,2001,53(3):159-168.
[18]Kaneshima S,Ando M.An analysis of split shear waves observed above crustal and uppermost mantle earthquakes beneath Shikoku,Japan:Implications in effective depth extent of seismic ani-sotropy[J].Journal of Geophysical Research:Solid Earth,1989,94(B10):14077-14092.
[19]Langston C A.Structure under Mount Rainier,Washington,inferred from teleseismic body waves[J].Journal of Geophysical Research:Solid Earth,1979,84(B9):4749-4762.
[20]Liu H,Niu F.Estimating crustal seismic anisotropy with a joint analysis of radial and transverse receiver function data[J].Geophysical Journal International,2012,188(1):144-164.
[21]Mc Namara D E,Owens T J.Azimuthal shear wave velocity anisotropy in the Basin and Range province using Moho Ps converted phases[J].Journal of Geophysical Research:Solid Earth,1993,98(B7):12003-12017.
[22]Nagaya M,Oda H,Akazawa H,et al.Receiver functions of seismic waves in layered anisotropic media:Application to the estimate of seismic anisotropy[J].Bulletin of the Seismological Society of America,2008,98(6):2990-3006.
[23]Nicolas A,Christensen N I.Formation of Anisotropy in Upper Mantle Peridotites‐A Review[J].Composition,structure and dynamics of the lithosphere-asthenosphere system,1987:111-123.
[24]Silver P G,Chan W W.Shear wave splitting and subcontinental mantle deformation[J].Journal of Geophysical Research:Solid Earth,1991,96(B10):16429-16454.
[25]Silver P G.Seismic anisotropy beneath the continents:probing the depths of geology[J].Annual review of earth and planetary sciences,1996,24:385-432.