地球科学进展 ›› 1995, Vol. 10 ›› Issue (6): 572 -576. doi: 10.11867/j.issn.1001-8166.1995.06.0572

干旱气候变化与可持续发展 上一篇    下一篇

地幔地球化学研究综述
王岳军 1,韩吟文 2,郑海飞 3   
  1. 1.中国科学院长沙大地构造所  长沙  410013;2.中国地质大学  武汉  430074;3.北京大学地质系  北京  100871
  • 收稿日期:1994-06-23 修回日期:1994-10-17 出版日期:1995-12-01
  • 通讯作者: 王岳军

REVIEW OF STUDIES ON MANTLE GEOCHEMISTRY

Wang Yueiun 1, Han Yinwen 2, Zheng Haifei 3   

  1. 1.Changsha Institute of Geotectonics, Academia Sinica, Changsha  410013;2.China University of Geoscience, Wuhan  430074;3.Beijing University, Beijing  100871
  • Received:1994-06-23 Revised:1994-10-17 Online:1995-12-01 Published:1995-12-01

系统地介绍了近二十年来地幔地球化学在全球及区域地幔平均化学组成,地幔的化学不均一性及区域矿产分布,地幔交代作用,化学地球动力学,地幔物理化学环境等五个方面的研究现状与进展。

This paper summarily reviews the progress and prospect of mantle geochemistry in the past two decades in studying:(1)The average composition of the whole and/or regional mantle in the Earth, (2) The relationship between mantle heterogeneity and regional distribution of deposits in the crust, (3) mantle metasomatism, (4)chemical geodynamics, and (5) Physico-chemical environment of the upper mantle.

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[1] 杨学明,杨晓勇,M.J.Le Bas. 碳酸岩的地质地球化学特征及其大地构造意义[J]. 地球科学进展, 1998, 13(5): 457-466.
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