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Lowermost mantle shear velocity anisotropy beneath Siberia

机译:西伯利亚以下的最低地幔剪切速度各向异性

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摘要

@@ IntroductionrnD"layer plays an important role in geodynamic process.And seismological research indicates that D"layer has large scale seismic anisotropy,however, most research concentrated on areas such as Northern Pacific,Central Pacific,Caribbean, Central America,Alaska etc.
机译:引言“ D”层在地球动力学过程中起着重要作用。地震研究表明,“ D”层具有较大的地震各向异性,然而,大多数研究集中在北太平洋,中太平洋,加勒比海,中美洲,阿拉斯加等地区。

著录项

  • 来源
    《地震学报(英文版)》 |2008年第2期|213-216|共4页
  • 作者单位

    School of Earth and Space Science, University of Science and Technology of China, Hefei 230026, China;

    School of Earth and Space Science, University of Science and Technology of China, Hefei 230026, China;

    School of Earth and Space Science, University of Science and Technology of China, Hefei 230026, China;

    School of Earth and Space Science, University of Science and Technology of China, Hefei 230026, China;

    School of Earth and Space Science, University of Science and Technology of China, Hefei 230026, China;

    School of Earth and Space Science, University of Science and Technology of China, Hefei 230026, China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类 地震波;
  • 关键词

    anisotropy; shear wave splitting; D" region; lowermost mantle; Siberia;

    机译:各向异性剪切波分裂D“地区;最低地幔;西伯利亚;
  • 入库时间 2022-08-19 03:55:21
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