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亚洲东部及边缘海地区背景噪声层析成像
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  • 英文篇名:Ambient noise surface wave tomography of marginal seas in east Asia
  • 作者:Q.Wang ; X.D.Song ; J.Y.Ren ; 王晴
  • 英文作者:Q.Wang;X.D.Song;J.Y.Ren;
  • 关键词:背景噪声层析成像 ; 亚洲东部 ; 莫霍面 ; 岩石层 ; 伸展
  • 中文刊名:DZYC
  • 英文刊名:Translated World Seismology
  • 机构:南京大学地球科学与工程学院;
  • 出版日期:2019-04-04
  • 出版单位:世界地震译丛
  • 年:2019
  • 期:v.50;No.303
  • 基金:国家自然科学基金(41774056,41772109);; 国家海洋局全球变化与海气相互作用专项(GASI-GEOGE-02)共同资助
  • 语种:中文;
  • 页:DZYC201903004
  • 页数:19
  • CN:03
  • ISSN:11-2368/P
  • 分类号:49-67
摘要
本文在亚洲东部地区进行了背景噪声层析成像的研究。研究区域包括中国东部沿海各省、朝鲜半岛、日本、台湾岛以及边缘海域。研究中收集了573个宽带台站的12个月的瑞利格林函数,从中提取了群速度和相速度频散曲线,编制了10~70s范围内的速度分布图,并通过反演获得了地壳和上地幔的三维剪切波速度模型。基于三维剪切波速度模型确定了研究区范围内的莫霍面深度和岩石层厚度。速度分布图显示在上地幔中存在三个明显的低速带,其中两个位于太平洋板块和菲律宾海板块俯冲带的增生楔内,另一个位于长白山和朝鲜半岛一带之下,上地幔岩石层在这些地区显著变薄。整个研究区域内的速度异常、地壳和岩石层厚度异常分布多呈NNE-SSW方向分布,在剖面图中岩石层显示出"香肠"状薄厚不一的形态。地壳和岩石层厚度均呈现出由NW向SE逐渐减薄的趋势,与中国东南部的多期次岩浆岩的分布相吻合。分析认为古太平洋板块俯冲以及伴随的多期次回撤是控制中国东部地壳伸展和岩石层减薄的主要动力因素。
        
引文
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