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地球科学进展  2002, Vol. 17 Issue (5): 685-692    DOI: 10.11867/j.issn.1001-8166.2002.05.0685
综述与评述     
玄武岩在研究岩石圈深部过程及构造背景中的应用
张树明1,2,王方正1
1.中国地质大学,湖北 武汉 430074;2.华东地质学院,江西 抚州 344000
BASALT'S ACTION ON RESEARCH GEOSPHERE DEEP-COURSE AND STRUCTURAL SETTING
ZHANG  Shu-ming1,2,  WANG  Fang-zheng1
1. China University of Geoscience,Wuhan 430074, China;2. East China Geological Institute, Fuzhou Jiangxi 344000,China
 全文: PDF(132 KB)  
摘要:

玄武岩在反演地幔物质成分、分析构造环境和岩石圈的深部动力学研究中具有重要意义。系统地综述了玄武岩的成因和岩浆源区性质、利用玄武岩判别地幔类型、玄武质岩浆的演化与大陆动力学关系,以及判别构造环境等方面研究的现状。阐述了研究中存在的问题,提出了今后的研究和发展方向,认为玄武岩研究应在大陆动力学研究中扮演重要角色。

关键词: 玄武岩岩石圈深部过程构造环境大陆动力学    
Abstract:

Basalt have importance meanings on deduce the Earth's mantle material composition, analysis  tectonic environment and the geosphere deep dynamics research. The paper based on synthesize domestic and  foreign's study achievement about basalt, systematical review basalt research history, present condition about basalt formation contributing factor and it's magma source area quality, uses the  basalt  to distinguish the Earth's mantle type, the connection basaltic magma's evolution and continent dynamics, and  uses the basalt to distinguish tectonic environment. Set forth the question on study basalt,put forward the orientation about research and develop on study basalt for the future,and ought to play an important role in study continent dynamics.

Key words: Basalt    Geosphere deep-course    Tectonic environment    Continent dynamics.
收稿日期: 2001-12-12 出版日期: 2002-10-01
:  P588.14+6   
基金资助:

国家自然科学基金项目“中国东部显生宙下地壳的形成与演化”(编号:40133020) 资助.

通讯作者: 张树明(1965-),男,江西抚州人,副教授,在职博士研究生,主要从事火成岩和基础地质研究及教学工作.E-mail:zsmfjxy@sohu.com     E-mail: zsmfjxy@sohu.com
作者简介: 张树明(1965-),男,江西抚州人,副教授,在职博士研究生,主要从事火成岩和基础地质研究及教学工作.E-mail:zsmfjxy@sohu.com
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引用本文:

张树明,王方正. 玄武岩在研究岩石圈深部过程及构造背景中的应用[J]. 地球科学进展, 2002, 17(5): 685-692.

ZHANG Shu-ming, WANG Fang-zheng. BASALT'S ACTION ON RESEARCH GEOSPHERE DEEP-COURSE AND STRUCTURAL SETTING. Advances in Earth Science, 2002, 17(5): 685-692.

链接本文:

http://www.adearth.ac.cn/CN/10.11867/j.issn.1001-8166.2002.05.0685        http://www.adearth.ac.cn/CN/Y2002/V17/I5/685

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