华北东北部裂陷盆地与燕山隆起地壳结构
|
摘要
天津—北京—赤城深地震测深剖面采用密集炮点和接收点距设计构成了较为完整的观测系统,利用该剖面地震测深资料研究华北东部裂陷盆地与燕山隆起地壳结构及构造耦合.结合该区域已有研究成果,进一步分析了张渤地震带东段的地震构造环境.结果显示,华北克拉通东部裂陷盆地结晶基底构造形态和界面结构性质与新生代以来的地壳构造运动密切相关,北侧燕山隆起区高速稳定和南侧裂陷盆地低速松散截然不同的地壳结构,使宝坻-桐柏、宁河-昌黎断裂构造分区线和燕山隆起之间的中间过渡带为张渤地震带东部平原区地震的孕发提供了良好的构造环境.
A comparatively complete layout chart is built by using small shot interval and receiver spacing in Tianjin-Beijing-Chicheng Deep Seismic Sounding profile.Based on the DSS data of the profile,the crustal structure and the tectonic coupling are studied in the rift-depression basin of eastern North China and Yanshan uplift.Combining with the existing research findings in the region,the seismic structure environment is further analyzed in the eastern segment of Zhangjiakou-Bohai seismic belt.The result shows that the tectonic feature and interface structure of the crystalline basement in the rift-depression basin of eastern North China Craton are correlated with the tectonic movement since Cenozoic era,The entirely different crustal structures between the stable Yanshan uplift with high velocity in the north and the incompact rift basin with low velocity in the south make the intergradational zone between the tectonic zoning line,Baodi-Tongbai and Ninghe-Changli faults,and Yanshan uplift provide a favorable structural environment for generation and occurrence of earthquakes in the eastern plain region of Zhangjiakou-Bohai seismic belt.
A comparatively complete layout chart is built by using small shot interval and receiver spacing in Tianjin-Beijing-Chicheng Deep Seismic Sounding profile.Based on the DSS data of the profile,the crustal structure and the tectonic coupling are studied in the rift-depression basin of eastern North China and Yanshan uplift.Combining with the existing research findings in the region,the seismic structure environment is further analyzed in the eastern segment of Zhangjiakou-Bohai seismic belt.The result shows that the tectonic feature and interface structure of the crystalline basement in the rift-depression basin of eastern North China Craton are correlated with the tectonic movement since Cenozoic era,The entirely different crustal structures between the stable Yanshan uplift with high velocity in the north and the incompact rift basin with low velocity in the south make the intergradational zone between the tectonic zoning line,Baodi-Tongbai and Ninghe-Changli faults,and Yanshan uplift provide a favorable structural environment for generation and occurrence of earthquakes in the eastern plain region of Zhangjiakou-Bohai seismic belt.
引文
[1]国家地震局《深部物探成果》编写组.中国地壳上地幔地球物理探测成果.北京:地震出版社,1986Results of Deep Geophysical Prospecting,Compile Group,State of Seismological Bureau.Results of Crustal and Upper Mantle by Deep Geophysical Prospecting in China(in Chinese).Beijing:Seismological Press,1986
[2]国家地震局科技监测司编.中国大陆深部构造的研究与进展.北京:地质出版社,1988Depart ment of Scientific Programming and Earthquake Monitoring,State of Seismological Bureau.Developments in the Research of Deep Structures of China′s Continent(in Chinese).Beijing:Geological Publishing House,1988
[3]刘昌铨,嘉世旭.唐山地震区地壳上地幔结构特征.地震学报,1986,8(4):341～353Liu C Q,Jia S X.Structural property of the crust and the upper mantle in the Tangshan earthquake region.Acta Seismologica Sinica,1986,8(4):1～22
[4]马杏垣,刘昌铨,刘国栋.江苏响水至内蒙古满都拉地学断面.北京:地质出版社,1991Ma X Y,Liu C Q,Liu G D.The Geoscience Transect from Xiangshui,Jiangsu Province to Mandal,Inner Monggola(in Chinese).Beijing:Geological Publishing House,1991
[5]孙武城,马宝林,宋松岩等.湖北随州至内蒙古喀喇沁旗地学断面.北京:地震出版社,1992Sun W C,Ma B L,Song S Y,et al.The GeoscienceTransect from Suizhou,Hubei Province to Kelaqinqi,Inner Monggola(in Chinese).Beijing:Seismological Press,1992
[6]刘昌铨,嘉世旭,刘明军.延庆—怀来盆地大震危险性分析研究.地震学报,1997,19(5):517～523Liu C Q,Jia S X,Liu MJ.Analysis and study of the large earthquake riskin Yanqing-Huailai basin.Acta Seismologica Sinica,1997,19(5):639～647
[7]张成科,张先康,盖玉杰等.文安—蔚县—察右中旗剖面地壳上地幔速度结构与构造研究.华北地震科学,1997,15(3):18～28Zhang C K,Zhang X K,Gai YJ,et al.Astudy of crust and upper mantle structure on Wen′an-Yuxian-Qahryouyizhongqi profile.North China Earthquake Science(in Chinese),1997,15(3):18～28
[8]王夫运,张先康,陈颙等.张渤构造带中段二维P波速度结构——安新—香河—宽城剖面.地震学报,2004,26(S1):31～41Wang F Y,Zhang X K,Chen Y,et al.2-D P-wave velocity structure in the mideast segment of Zhangjiakou-Bohai tectonic zone:Anxin-Xianghe-Kuancheng DSS profile.Acta Seismologica Sinica(in Chinese),2004,26(S1):31～41
[9]朱露培,曾融生,刘福田.京津唐张地区地壳上地幔三维P波速度结构.地球物理学报,1990,33(3):267～277Zhu L P,Zeng R S,Liu F T.Three-dimensional P-wave velocity structure under the Beijing network area.Chinese J.Geophys.(in Chinese),1990,33(3):267～277
[10]孙若昧,刘福田.京津唐地区地壳结构与强震发生——I.P波速度结构.地球物理学报,1995,38(5):599～607Sun R M,Liu F T.Crust structure and strong earthquake in Beijing,Tianjing,Tangshan area:I.P wave velocity structure.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1995,38(5):599～607
[11]Huang J L,Zhao D P.Crustal heterogeneity and seismotectonics of the region around Beijing China.Tectonophysics,2004,385:159～180
[12]于湘伟,陈运泰,王培德.京津唐地区中上地壳三维P波速度结构.地震学报,2003,25(1):1～14Yu X W,Chen Y T,Wang P D.Three-dimensional P wave velocity structure in Beijing-Tianjin-Tangshan area.Acta Seismologica Sinica(in Chinese),2003,25(1):1～14
[13]齐诚,赵大鹏,陈颙等.首都圈地区地壳P波和S波三维速度结构及其与大地震的关系.地球物理学报,2006,49(3):805～815Qi C,Zhao D P,Chen Y,et al.3-D P and S wave velocity structures and their relationship to strong earthquakes in the Chinese capital region.Chinese J.Geophys.(in Chinese),2006,49(3):805～815
[14]李志伟,胥颐,郝天珧等.环渤海地区的地震层析成像与地壳上地幔结构.地球物理学报,2006,49(3):797～804Li Z W,Xu Y,Hao T Y,et al.Seismic tomography and velocity structure in the crust and upper mantle around Bohai Area.Chinese J.Geophys.(in Chinese),2006,49(3):797～804
[15]嘉世旭,张先康,方盛明.华北裂陷盆地不同块体地壳结构及演化研究.地学前缘,2001,8(2):259～266Jia S X,Zhang X K,Fang S M.Research on the crustal structure and evolution of different blocksin North China rift-depression basin.Earth Science Frontiers(in Chinese),2001,8(2):259～266
[16]杨理华,刘德林,赵喜柱等.北京、天津、河北地震构造.见:马杏垣主编.中国岩石圈动力学地图集.北京:中国地图出版社,1989,30Yang L H,Liu D L,Zhao X Z,et al.Seismotectonics of Hebei Province including Beijing and Tianjin.In:Ma Xingyuan ed.Lithospheric Dynamics Atlas of China(in Chinese).Beijing:China Cartographic Publishing House,1989.30
[17]嘉世旭,刘昌铨.华北地区人工地震测深震相与地壳结构研究.地震地质,1995,17(2):97～105Jia S X,Liu C Q.Study onthe seismic phase of DSSin north China.Seismology and Geology(in Chinese),1995,17(2):97～105
[18]Cervny V,Psencik I.SEIS83-numerical modeling of seismic wavefield in2-D laterally varying layered structures by the ray method.In:Engdahl E R ed.Documentation of Earthquake Algorithm.Boulder Colo Rep:World Data Center for Solid Earth Geohpysical,SE-35,1984.36～40
[19]嘉世旭,刘昌铨.动力学射线追踪方法及其在二维非均匀介质理论地震图计算中的应用.见:中国大陆深部构造的研究与进展.北京:地质出版社,1988.279～287Jia S X,Liu C Q.Dynamic ray tracing and its application to the computation of synthetic seismograms in2-D heterogeneous medium.In:Developments in the Research of Deep Structures of China′s Continent(in Chinese).Beijing:Geological Publishing House,1988.324～335
[20]Banda E,Deichman N,Braile L W,et al.Amplitude study of the Pg phase.Journal of Geophysics,1982,51:153～164
[21]嘉世旭,张先康.华北不同构造块体地壳结构及其对比研究.地球物理学报,2005,48(3):611～620Jia S X,Zhang X K.Crustal structure and comparison of different tectonic blocks in North China.Chinese J.Geophys.(in Chinese),2005,48(3):672～683
[22]嘉世旭,齐诚,王夫运等.首都圈地壳网格化三维结构.地球物理学报,2005,48(6):1316～1324Jia S X,Qi C,Wang F Y,et al.Three-dimensional crustal gridding structure of the capital area.Chinese J.Geophys.(in Chinese),2005,48(6):1397～1407
[23]邓起东主编.中国活动构造图.北京:地震出版社,2007年2月Deng Q D ed.Map of Active Tectonics in China(in Chinese).Beijing:Seismological Press,2007.2
[24]梅世蓉.地震前兆场物理模式与前兆时空分布机制研究(一)—坚固体孕震模式的由来与证据.地震学报,1995,17(3):273～282Mei S R.On the physical model of earthquake precursor fields and the mechanism of precursors′Time-Space distribution—Origin and evidences of the strong bodyearthquake-generating model.Acta Seismologica Sinica,1986,8(4):1～22
[25]陈宇坤,聂永安.坚固体模型近地表形变场、应力场时空分布动态模拟研究.西北地震学报,2001,23(4):105～111Chen Y K,Nie Y A.Dynamic simulation on space-time distribution of deformation and stree fields near surface in hard-inclusion earthquake preparation model.Northwestern Seismological Journal(in Chinese),2001,23(4):105～111
[2]国家地震局科技监测司编.中国大陆深部构造的研究与进展.北京:地质出版社,1988Depart ment of Scientific Programming and Earthquake Monitoring,State of Seismological Bureau.Developments in the Research of Deep Structures of China′s Continent(in Chinese).Beijing:Geological Publishing House,1988
[3]刘昌铨,嘉世旭.唐山地震区地壳上地幔结构特征.地震学报,1986,8(4):341～353Liu C Q,Jia S X.Structural property of the crust and the upper mantle in the Tangshan earthquake region.Acta Seismologica Sinica,1986,8(4):1～22
[4]马杏垣,刘昌铨,刘国栋.江苏响水至内蒙古满都拉地学断面.北京:地质出版社,1991Ma X Y,Liu C Q,Liu G D.The Geoscience Transect from Xiangshui,Jiangsu Province to Mandal,Inner Monggola(in Chinese).Beijing:Geological Publishing House,1991
[5]孙武城,马宝林,宋松岩等.湖北随州至内蒙古喀喇沁旗地学断面.北京:地震出版社,1992Sun W C,Ma B L,Song S Y,et al.The GeoscienceTransect from Suizhou,Hubei Province to Kelaqinqi,Inner Monggola(in Chinese).Beijing:Seismological Press,1992
[6]刘昌铨,嘉世旭,刘明军.延庆—怀来盆地大震危险性分析研究.地震学报,1997,19(5):517～523Liu C Q,Jia S X,Liu MJ.Analysis and study of the large earthquake riskin Yanqing-Huailai basin.Acta Seismologica Sinica,1997,19(5):639～647
[7]张成科,张先康,盖玉杰等.文安—蔚县—察右中旗剖面地壳上地幔速度结构与构造研究.华北地震科学,1997,15(3):18～28Zhang C K,Zhang X K,Gai YJ,et al.Astudy of crust and upper mantle structure on Wen′an-Yuxian-Qahryouyizhongqi profile.North China Earthquake Science(in Chinese),1997,15(3):18～28
[8]王夫运,张先康,陈颙等.张渤构造带中段二维P波速度结构——安新—香河—宽城剖面.地震学报,2004,26(S1):31～41Wang F Y,Zhang X K,Chen Y,et al.2-D P-wave velocity structure in the mideast segment of Zhangjiakou-Bohai tectonic zone:Anxin-Xianghe-Kuancheng DSS profile.Acta Seismologica Sinica(in Chinese),2004,26(S1):31～41
[9]朱露培,曾融生,刘福田.京津唐张地区地壳上地幔三维P波速度结构.地球物理学报,1990,33(3):267～277Zhu L P,Zeng R S,Liu F T.Three-dimensional P-wave velocity structure under the Beijing network area.Chinese J.Geophys.(in Chinese),1990,33(3):267～277
[10]孙若昧,刘福田.京津唐地区地壳结构与强震发生——I.P波速度结构.地球物理学报,1995,38(5):599～607Sun R M,Liu F T.Crust structure and strong earthquake in Beijing,Tianjing,Tangshan area:I.P wave velocity structure.Chinese J.Geophys.(Acta Geophysica Sinica)(in Chinese),1995,38(5):599～607
[11]Huang J L,Zhao D P.Crustal heterogeneity and seismotectonics of the region around Beijing China.Tectonophysics,2004,385:159～180
[12]于湘伟,陈运泰,王培德.京津唐地区中上地壳三维P波速度结构.地震学报,2003,25(1):1～14Yu X W,Chen Y T,Wang P D.Three-dimensional P wave velocity structure in Beijing-Tianjin-Tangshan area.Acta Seismologica Sinica(in Chinese),2003,25(1):1～14
[13]齐诚,赵大鹏,陈颙等.首都圈地区地壳P波和S波三维速度结构及其与大地震的关系.地球物理学报,2006,49(3):805～815Qi C,Zhao D P,Chen Y,et al.3-D P and S wave velocity structures and their relationship to strong earthquakes in the Chinese capital region.Chinese J.Geophys.(in Chinese),2006,49(3):805～815
[14]李志伟,胥颐,郝天珧等.环渤海地区的地震层析成像与地壳上地幔结构.地球物理学报,2006,49(3):797～804Li Z W,Xu Y,Hao T Y,et al.Seismic tomography and velocity structure in the crust and upper mantle around Bohai Area.Chinese J.Geophys.(in Chinese),2006,49(3):797～804
[15]嘉世旭,张先康,方盛明.华北裂陷盆地不同块体地壳结构及演化研究.地学前缘,2001,8(2):259～266Jia S X,Zhang X K,Fang S M.Research on the crustal structure and evolution of different blocksin North China rift-depression basin.Earth Science Frontiers(in Chinese),2001,8(2):259～266
[16]杨理华,刘德林,赵喜柱等.北京、天津、河北地震构造.见:马杏垣主编.中国岩石圈动力学地图集.北京:中国地图出版社,1989,30Yang L H,Liu D L,Zhao X Z,et al.Seismotectonics of Hebei Province including Beijing and Tianjin.In:Ma Xingyuan ed.Lithospheric Dynamics Atlas of China(in Chinese).Beijing:China Cartographic Publishing House,1989.30
[17]嘉世旭,刘昌铨.华北地区人工地震测深震相与地壳结构研究.地震地质,1995,17(2):97～105Jia S X,Liu C Q.Study onthe seismic phase of DSSin north China.Seismology and Geology(in Chinese),1995,17(2):97～105
[18]Cervny V,Psencik I.SEIS83-numerical modeling of seismic wavefield in2-D laterally varying layered structures by the ray method.In:Engdahl E R ed.Documentation of Earthquake Algorithm.Boulder Colo Rep:World Data Center for Solid Earth Geohpysical,SE-35,1984.36～40
[19]嘉世旭,刘昌铨.动力学射线追踪方法及其在二维非均匀介质理论地震图计算中的应用.见:中国大陆深部构造的研究与进展.北京:地质出版社,1988.279～287Jia S X,Liu C Q.Dynamic ray tracing and its application to the computation of synthetic seismograms in2-D heterogeneous medium.In:Developments in the Research of Deep Structures of China′s Continent(in Chinese).Beijing:Geological Publishing House,1988.324～335
[20]Banda E,Deichman N,Braile L W,et al.Amplitude study of the Pg phase.Journal of Geophysics,1982,51:153～164
[21]嘉世旭,张先康.华北不同构造块体地壳结构及其对比研究.地球物理学报,2005,48(3):611～620Jia S X,Zhang X K.Crustal structure and comparison of different tectonic blocks in North China.Chinese J.Geophys.(in Chinese),2005,48(3):672～683
[22]嘉世旭,齐诚,王夫运等.首都圈地壳网格化三维结构.地球物理学报,2005,48(6):1316～1324Jia S X,Qi C,Wang F Y,et al.Three-dimensional crustal gridding structure of the capital area.Chinese J.Geophys.(in Chinese),2005,48(6):1397～1407
[23]邓起东主编.中国活动构造图.北京:地震出版社,2007年2月Deng Q D ed.Map of Active Tectonics in China(in Chinese).Beijing:Seismological Press,2007.2
[24]梅世蓉.地震前兆场物理模式与前兆时空分布机制研究(一)—坚固体孕震模式的由来与证据.地震学报,1995,17(3):273～282Mei S R.On the physical model of earthquake precursor fields and the mechanism of precursors′Time-Space distribution—Origin and evidences of the strong bodyearthquake-generating model.Acta Seismologica Sinica,1986,8(4):1～22
[25]陈宇坤,聂永安.坚固体模型近地表形变场、应力场时空分布动态模拟研究.西北地震学报,2001,23(4):105～111Chen Y K,Nie Y A.Dynamic simulation on space-time distribution of deformation and stree fields near surface in hard-inclusion earthquake preparation model.Northwestern Seismological Journal(in Chinese),2001,23(4):105～111
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心