用户名: 密码: 验证码:
松辽盆地北缘的上地幔速度结构及该区火山成因探讨
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Velocity structure in upper mantle and its implications for the volcanism nearby the north edge of Songliao Basin
  • 作者:张风雪 ; 吴庆举
  • 英文作者:ZHANG FengXue;WU QingJu;Institute of Geophysics,China Earthquake Administration;Key Laboratory of Seismic Observation and Geophysical Imaging,Institute of Geophysics,China Earthquake Administration;
  • 关键词:诺敏河 ; 五大连池 ; 火山活动 ; 层析成像
  • 英文关键词:Nuomin River;;Wudalianchi;;Volcanism;;Tomography
  • 中文刊名:DQWX
  • 英文刊名:Chinese Journal of Geophysics
  • 机构:中国地震局地球物理研究所;中国地震局地球物理研究所地震观测与地球物理成像重点实验室;
  • 出版日期:2019-08-12
  • 出版单位:地球物理学报
  • 年:2019
  • 期:v.62
  • 基金:国家自然科学基金(41474074,41874072,41674103,41304066)资助
  • 语种:中文;
  • 页:DQWX201908014
  • 页数:12
  • CN:08
  • ISSN:11-2074/P
  • 分类号:140-151
摘要
中国东北是研究板内新生代火山活动及其成因的天然场所.以往的研究根据不同的壳幔速度结构,提出多种模型用以解释中国东北地区的火山活动.由于松辽盆地北缘的观测台站相对较少,导致这些模型对盆地北缘的约束较弱.我们利用近年来覆盖松辽盆地北缘的流动宽频带观测台站数据开展远震体波走时层析成像研究,获得了深达800km的深部速度结构,在盆地北缘的火山群区域内得到如下认识:诺敏河和五大连池火山群共用一个200~300km深处的地幔岩浆房.该地幔岩浆房内的低速异常为水平展布,未下延至地幔转换带内,并仅在该区域上地幔的局部范围内有所体现.结合前人的研究结果分析,我们认为该水平的局部低速异常可能是中生代晚期岩石圈拆沉导致的软流圈上涌热物质.
        Northeast China is a natural experimental site for studying Cenozoic intraplate volcanism.On the basis of crustal and mantle velocity structures,several models for volcanism in this region have been proposed in previous studies.However,these models pose a weak constraint on the volcanism in north edge of Songliao Basin due to few seismic stations.We conducted a tomographic study using teleseismic body wave traveltime recorded by broadband seismic stations covering the north edge of Songliao Basin,and inverted the traveltime residuals to image crustal and mantle structure down to 800 km depth.Results show that the Nuomin River and Wudalianchi volcanic group share a common mantle magma chamber at 200~300 km depth beneath volcanic cones.The magma chamber shows a slow velocity anomaly in the horizontal direction,and only exists in a local area within the upper mantle that does not extend down to the mantle transition zone.Combined with previous work,we suggest that this horizontal low velocity structure resulted from asthenospheric upwelling triggered by lithospheric delamination during late Mesozoic.
引文
Data Management Centre of China National Seismic Network.2007.Waveform data of China National Seismic Network.Institute of Geophysics,China Earthquake Administration.http:∥www.seisdmc.ac.cn.
    Fan Q C,Sui J L,Sun Q,et al.2005.Preliminary research of magma mixing and explosive mechanism of the Millennium eruption of Tianchi volcano.Acta Petrologica Sinica(in Chinese),21(6):1703-1708.
    Fan Q C,Zhao Y W,Sui J L,et al.2012.Studies on Quaternary volcanism stages of Nuomin river area in the Great Xing′an Range:Evidence from petrology,K-Ar dating and volcanic geology features.Acta Petrologica Sinica(in Chinese),28(4):1092-1098.
    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,doi:10.1016/j.epsl.2015.01.044.
    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,doi:10.1016/j.epsl.2015.09.035.
    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.
    Julian B R,Gubbins D.1977.Three-dimensional seismic ray tracing.Journal of Geophysics,43:95-113.
    Kim S,Tkalcic′H,Rhie J,et al.2016.Intraplate volcanism controlled by back-arc and continental structures in NE Asia inferred from transdimensional Bayesian ambient noise tomography.Geophysical Research Letters,43(16):8390-8398,doi:10.1002/2016GL069483.
    Kuritani T,Kimura J I,Ohtani E,et al.2013.Transition zone origin of potassic basalts from Wudalianchi volcano,northeast China.Lithos,156-159:1-12,doi:10.1016/j.lithos.2012.10.010.
    Laske G,Masters G,Ma Z T,et al.2013.Update on CRUST1.0-A 1-degree Global Model of Earth′s Crust.EGU General Assembly,15:2658.
    Lei J S,Zhao D P.2005.P-wave tomography and origin of the Changbai intraplate volcano in Northeast Asia.Tectonophysics,397(3-4):281-295,doi:10.1016/j.tecto.2004.12.009.
    Li C,Van Der Hilst R D.2010.Structure of the upper mantle and transition zone beneath Southeast Asia from traveltime tomography.Journal of Geophysical Research:Solid Earth,115(B7):B07308,doi:10.1029/2009JB006882.
    Li N,Zhang L Y,Zhao Y W,et al.2012.Genesis of potassic minerals in the Xiaogulihe-Keluo-Wudalianchi-Erkeshan volcanic rock belt,Northeast China and their geological implications.Acta Petrologica Sinica(in Chinese),28(4):1173-1180.
    Li Z W,Ni S D,Zhang B L,et al.2016.Shallow magma chamber under the Wudalianchi Volcanic Field unveiled by seismic imaging with dense array.Geophysical Research Letters,43(10):4954-4961,doi:10.1002/2016GL068895.
    Liu R X,Fan Q C,Zheng X S,et al.1998.The magma evolution of Tianchi volcano,Changbaishan.Science in China Series D:Earth Sciences,41(4):382-389.
    Ma J C,Tian Y,Liu C,et al.2018.P-wave tomography of Northeast Asia:constraints on the western Pacific plate subduction and mantle dynamics.Physics of the Earth and Planetary Interiors,274:105-126,doi:10.1016/j.pepi.2017.11.003.
    Paige C C,Saunders M A.1982a.LSQR:An algorithm for sparse linear equations and sparse least squares.ACM Transactions on Mathematical Software,8(1):43-71.
    Paige C C,Saunders M A.1982b.Algorithm 583LSQR:Sparse linear equations and least squares problems.ACM Transactions on Mathematical Software,8(2):195-209.
    Pan J T,Li Y H,Wu Q J,et al.2014.3-D S-wave velocity structure of crust and upper-mantle beneath the northeast China.Chinese J.Geophys.(in Chinese),57(7):2077-2087,doi:10.6038/cjg20140705.
    Qiang Z Y,Wu Q J.2015.Upper mantle anisotropy beneath the north of northeast China and its dynamic significance.Chinese J.Geophys.(in Chinese),58(10):3540-3552,doi:10.6038/cjg20151010.
    Qiang Z Y,Wu Q J.2019.Lithospheric deformation of the Nuomin River volcano in Northeast China:Evidence from shear wave splitting.Chinese J.Geophys.(in Chinese),62(1):104-114,doi:10.6038/cjg2019M0134.
    Rawlinson N,Kennett B L N.2004.Rapid estimation of relative and absolute delay times across a network by adaptive stacking.Geophys.J.Int.,157(1):332-340,doi:10.1111/j.1365-246X.2004.02188.x.
    Rawlinson N,Reading A M,Kennett B L N.2006.Lithospheric structure of Tasmania from a novel form of teleseismic tomography.Journal of Geophysical Research:Solid Earth,111(B2):B02301,doi:10.1029/2005JB003803.
    Tang Y C,Obayashi M,Niu F L,et al.2014.Changbaishan volcanism in northeast China linked to subduction-induced mantle upwelling.Nature Geoscience,7(6):470-475,doi:10.1038/NGEO2166.
    Tao K,Grand S P,Niu F L.2018.Seismic structure of the upper mantle beneath eastern Asia from full waveform seismic tomography.Geochem.Geophys.Geosyst.,19(8):2732-2763,doi:10.1029/2018GC007460.
    Tian Y,Hung S H,Nolet G,et al.2007.Dynamic ray tracing and traveltime corrections for global seismic tomography.Journal of Computational Physics,226(1):672-687,doi:10.1016/j.jcp.2007.04.025.
    Tian Y,Ma J C,Liu C,et al.2019.Effects of subduction of the western Pacific plate on tectonic evolution of Northeast China and geodynamic implications.Chinese J.Geophys.(in Chinese),62(3):1071-1082,doi:10.6038/cjg2019M0061.
    VanDecar J C,Crosson R S.1990.Determination of teleseismic relative phase arrival times using multi-channel cross-correlation and least squares.Bulletin of the Seismological Society of America,80(1):150-169.
    Wang F,Zhou X H,Zhang L C,et al.2006.Late mesozoic volcanism in the Great Xing′an Range(NE China):Timing and implications for the dynamic setting of NE Asia.Earth and Planetary Science Letters,251(1-2):179-198,doi:10.1016/j.epsl.2006.09.007.
    Wei W,Xu J D,Zhao D P,et al.2012.East Asia mantle tomography:New insight into plate subduction and intraplate volcanism.Journal of Asian Earth Sciences,60:88-103,doi:10.1016/j.jseaes.2012.08.001.
    Wei W,Hammond J O S,Zhao D P,et al.2019.Seismic evidence for a mantle transition zone origin of the wudalianchi and Halaha volcanoes in Northeast China.Geochem.Geophys.Geosyst.,20(1):398-416,doi:10.1029/2018GC007663.
    Xie Z X,Wu Q J,Zhou S Y,et al.2018.Study of crustal thickness and Vp/Vsratio beneath the Nuomin River volcanoes.Chinese J.Geophys.(in Chinese),61(12):4805-4816,doi:10.6038/cjg2018M0197.
    Zhang F X,Wu Q J,Li Y H.2013a.The traveltime tomography study by teleseismic P wave data in the Northeast China area.Chinese J.Geophys.(in Chinese),56(8):2690-2700,doi:10.6038/cjg20130818.
    Zhang F X,Wu Q J,Li Y H,et al.2013b.Pick up the teleseismic relative traveltime residuals by wave form correlation based on the GUI.Seismological and Geomagnetic Observation and Research(in Chinese),34(3-4):58-64,doi:10.3969/j.issn.1003-3246.2013.03/04.012.
    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,doi:10.1016/j.chemgeo.2010.05.013.
    Zhao D P,Hasegawa A,Horiuchi S.1992.Tomographic imaging of Pand S wave velocity structure beneath Northeastern Japan.Journal of Geophysical Research:Solid Earth,97(B13):19909-19928.
    Zhao D P,Tian Y,Lei J S,et al.2009.Seismic image and origin of the Changbai intraplate volcano in East Asia:Role of big mantle wedge above the stagnant Pacific slab.Physics of the Earth and Planetary Interiors,173(3-4):197-206,doi:10.1016/j.pepi.2008.11.009.
    Zhao Y W,Fan Q C,Bai Z D,et al.2013.Quaternary volcanism in the Nuomin River and Kuile River area of the Greater Hinggan Mountains.Science China Earth Sciences,56(2):173-181,doi:10.1007/s11430-012-4544-7.
    Zhao Y W,Fan Q C,Zou H B,et al.2014a.Geochemistry of Quaternary basaltic lavas from the Nuomin volcanic field,Inner Mongolia:Implications for the origin of potassic volcanic rocks in Northeastern China.Lithos,196-197:169-180,doi:10.1016/j.lithos.2014.03.011.
    Zhao Y W,Li N,Fan Q C,et al.2014b.Two episodes of volcanism in the Wudalianchi volcanic belt,NE China:Evidence for tectoniccontrols on volcanic activities.Journal of Volcanology and Geothermal Research,285:170-179,doi:10.1016/j.jvolgeores.2014.08.016.
    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 J.Geophys.(in Chinese),52(5):1412-1417,doi:10.3969/j.issn.0001-5733.2009.05.031.
    樊祺诚,隋建立,孙谦等.2005.天池火山千年大喷发的岩浆混合作用与喷发机制初步探讨.岩石学报,21(6):1703-1708.
    樊祺诚,赵勇伟,隋建立等.2012.大兴安岭诺敏河第四纪火山岩分期:岩石学、年代学与火山地质特征.岩石学报,28(4):1092-1098.
    国家测震台网数据备份中心.2007.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.
    李霓,张柳毅,赵勇伟等.2012.我国东北小古里河-科洛-五大连池-二克山火山带钾质矿物成因及地质意义.岩石学报,28(4):1173-1180.
    刘若新,樊祺诚,郑祥身等.1998.长白山天池火山的岩浆演化.中国科学(D辑),28(3):226-231.
    潘佳铁,李永华,吴庆举等.2014.中国东北地区地壳上地幔三维S波速度结构.地球物理学报,57(7):2077-2087,doi:10.6038/cjg20140705.
    强正阳,吴庆举.2015.中国东北地区北部上地幔各向异性及其动力学意义.地球物理学报,58(10):3540-3552,doi:10.6038/cjg20151010.
    强正阳,吴庆举.2019.中国东北诺敏河火山岩石圈变形:来自剪切波分裂的证据.地球物理学报,62(1):104-114,doi:10.6038/cjg2019M0134.
    田有,马锦程,刘财等.2019.西太平洋俯冲板块对中国东北构造演化的影响及其动力学意义.地球物理学报,62(3):1071-1082,doi:10.6038/cjg2019M0061.
    谢振新,吴庆举,周仕勇等.2018.兴蒙造山带诺敏河火山群地壳厚度与波速比研究.地球物理学报,61(12):4805-4816,doi:10.6038/cjg2018M0197.
    张风雪,吴庆举,李永华.2013a.中国东北地区远震P波走时层析成像研究.地球物理学报,56(8):2690-2700,doi:10.6038/cjg20130818.
    张风雪,吴庆举,李永华等.2013b.基于图形界面的波形相关法拾取远震相对走时残差.地震地磁观测与研究,34(3-4):58-64,doi:10.3969/j.issn.1003-3246.2013.03/04.012.
    赵勇伟,樊祺诚,白志达等.2013.大兴安岭诺敏河-奎勒河地区第四纪火山活动研究.中国科学:地球科学,43(9):1464-1473.
    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.

© 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