| 利用瑞雷面波反演华北克拉通东北部边界的岩石圈结构 |
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| 引用本文： | 李明明,何玉梅.利用瑞雷面波反演华北克拉通东北部边界的岩石圈结构[J].地震学报,2011,33(2):143-155. |
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| 作者姓名： | 李明明 何玉梅 |
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| 作者单位： | 1 ）中国北京 100029 中国科学院地质与地球物理研究所
2 ）中国北京 100049中国科学院研究生院地球科学学院 |
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| 基金项目： | 国家自然科学基金项目，国家自然科学基金重大研究计划 |
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| 摘 要： | 运用瑞雷面波相速度频散曲线分析和反演得到了华北克拉通东北部边界及其邻近区域岩石圈的精细S波速度结构.利用11个地震事件、60个台站的瑞雷面波波形资料,得到了周期从25-150 S的相速度频散曲线,并且通过线性反演方法得到了深度从40-300 km的S波速度结构.结果表明,该研究区域S波速度存在强烈的不均匀性.从东南部的...
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| 关 键 词： | 瑞雷面波 华北克拉通 索伦缝合带 岩石圈 |
Lithospheric structure beneath northeastern boundary region of the North China Craton from Rayleigh wave dispersion inversion |
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| Li Mingming,He YumeiInstitute of Geology , Geophysics,Chinese Academy of Sciences,Beijing ,ChinaCollege of Earth Science,Graduate University of Chinese Academy of Sciences,Beijing ,China.Lithospheric structure beneath northeastern boundary region of the North China Craton from Rayleigh wave dispersion inversion[J].Acta Seismologica Sinica,2011,33(2):143-155. |
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| Authors: | Li Mingming He YumeiInstitute of Geology Geophysics Chinese Academy of Sciences Beijing ChinaCollege of Earth Science Graduate University of Chinese Academy of Sciences Beijing China |
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| Institution: | 1)Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China2)College of Earth Science, Graduate University of Chinese Academy of Sciences, Beijing 100049, Chinabusiness week la |
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| Abstract: | We have inverted Rayleigh wave dispersion data to produce a high resolution image of the S-wave velocity structure of the lithosphere beneath northeast boundary region of the North China Craton and adjacent areas.Based on waveform data recorded from 60 stations and 11 events,Rayleigh wave phase velocities were measured at periods from 25 to 150 s.The phase velocities were utilized in subsequent inversion to solve for the S-wave velocity structure from 40 km down to 300 km depth.The result shows strong later... |
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| Keywords: | Rayleigh wave North China Craton Solonker suture lithosphere |
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