地球科学进展 ›› 2005, Vol. 20 ›› Issue (10): 1095 -1099. doi: 10.11867/j.issn.1001-8166.2005.10.1095

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热柱、超级热柱及其成因的研究进展
谢鸿森,侯渭,周文戈   
  1. 中国科学院地球化学研究所,贵州 贵阳 550002
  • 收稿日期:2004-11-02 修回日期:2005-06-13 出版日期:2005-10-25
  • 通讯作者: 谢鸿森
  • 基金资助:

    国家自然科学基金重大项目“地球内部几个重要界面物质的高温高压物性研究”(编号:10299040);中国科学院知识创新工程重要方向项目“同步辐射高压高温实验技术及地幔地核重要矿物的物性研究”(编号:KJCX2-SW-No.3)资助.

DEVELOPMENT OF STUDIES OF PLUME, SUPERPLUME AND THEIR ORIGIN

XIE Hongsen; HOU Wei; ZHOU Wenge   

  1. Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002,China
  • Received:2004-11-02 Revised:2005-06-13 Online:2005-10-25 Published:2005-10-25

从20世纪地幔热柱假说问世,经过30多年的发展,在地幔热柱的全球分布、鉴别特征、形态学和成因理论方面都有了长足的进步。特别是通过下地幔不均匀性的研究,发现了下地幔中存在的超级热柱和下地幔底层中的超低速带,为探讨热柱成因提供了重要依据。

In the last thirties years great advances of the studies of mantle plumes have been made. Based on the depth of origin, the mantle plumes have been subdivided into three groups. These are deep plume, transition zone origin plume and uppermantle plume. In this paper the criteria used to diagnose deep plumes and transition zone origin plumes are induced. The distribution of these plumes around the Earth surface and their shape are described. In addition, the superplumes in lower mantle and ultra-low velocity zones in mostly lower mantle found by the investigation of seismic tomography give an important evidence for the origin of plumes.

中图分类号: 

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