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The v_P Velocity Structures of Sub-blocks in the North China Craton from Active Source Waveform Modeling and Tectonic Implications
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  • 英文篇名:The v_P Velocity Structures of Sub-blocks in the North China Craton from Active Source Waveform Modeling and Tectonic Implications
  • 作者:LIU ; Hanqi ; TIAN ; Xiaofeng ; LIU ; Baofeng ; WANG ; Honglei
  • 英文作者:LIU Hanqi;TIAN Xiaofeng;LIU Baofeng;WANG Honglei;Geophysical Exploration Center,China Earthquake Administration;Hebei Earthquake Agency;
  • 英文关键词:The North China Craton;;Crustal velocity structure;;Craton destructure;;Wide-angle reflection/refraction
  • 中文刊名:ZDZW
  • 英文刊名:中国地震研究(英文版)
  • 机构:Geophysical Exploration Center,China Earthquake Administration;Hebei Earthquake Agency;
  • 出版日期:2019-05-15
  • 出版单位:Earthquake Research in China
  • 年:2019
  • 期:v.33
  • 基金:This project sponsored by the National Natural Science Foudation of China(NSFC)(41574084 and 41774071)
  • 语种:英文;
  • 页:ZDZW201902010
  • 页数:12
  • CN:02
  • ISSN:11-2009/P
  • 分类号:114-125
摘要
We present the 1-D crustal velocity structure of the major tectonic blocks of the North China Craton(NCC) along 36°N based on synthetic seismogram modeling of long-range wide-angle reflection/refraction data. This profile extends from southwest Yan'an of central Shaanxi Province of China(109.47°E), across the southern Trans-North China Orogen(TNCO), the southwestern part of the North China Plain(NCP), the Luxi Uplift(LU) and the Sulu Orogen(SLO), ending at Qingdao City of Shandong Province, the eastern margin of China(120.12°E) along 36°N. We utilized reflectivity synthetic seismogram modeling of the active source data to develop 1-D velocity structures of the sub-blocks of the NCC. Our final model shows that the NCC crust varies remarkably among the tectonic units with different velocity structure features. Higher lower crustal velocity and Moho depth ~42 km is a major feature of the crust beneath southern Ordos Blockt. The TNCO which is composed of Lyuliangshan Mountains(LM), Shanxi Graben(SXG) and Taihangshan Mountains(TM) shows dominant trans-orogenic features. The NCP shows a dominant thickening of sediments, sharp crust thinning with Moho depth ~32 km and significant lower average velocity. The SLO and the LU shows a stratified crust, higher average velocity and crust thinning with Moho depth of ~35 km. Our model shows the coincidence between the deep structure and the surface geology among all the tectonic sub-blocks of the NCC.
        We present the 1-D crustal velocity structure of the major tectonic blocks of the North China Craton(NCC) along 36°N based on synthetic seismogram modeling of long-range wide-angle reflection/refraction data. This profile extends from southwest Yan'an of central Shaanxi Province of China(109.47°E), across the southern Trans-North China Orogen(TNCO), the southwestern part of the North China Plain(NCP), the Luxi Uplift(LU) and the Sulu Orogen(SLO), ending at Qingdao City of Shandong Province, the eastern margin of China(120.12°E) along 36°N. We utilized reflectivity synthetic seismogram modeling of the active source data to develop 1-D velocity structures of the sub-blocks of the NCC. Our final model shows that the NCC crust varies remarkably among the tectonic units with different velocity structure features. Higher lower crustal velocity and Moho depth ~42 km is a major feature of the crust beneath southern Ordos Blockt. The TNCO which is composed of Lyuliangshan Mountains(LM), Shanxi Graben(SXG) and Taihangshan Mountains(TM) shows dominant trans-orogenic features. The NCP shows a dominant thickening of sediments, sharp crust thinning with Moho depth ~32 km and significant lower average velocity. The SLO and the LU shows a stratified crust, higher average velocity and crust thinning with Moho depth of ~35 km. Our model shows the coincidence between the deep structure and the surface geology among all the tectonic sub-blocks of the NCC.
引文
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