中国地质调查局西安地质调查中心主办
高级检索

中国西北大陆岩石圈类型、岩石学结构及其意义

,  ,  ,  ,  ,  ,  ,  ,  ,  ,  , 

文章导航 > 西北地质 > 2008 > 41(2): 1-21

上一篇

下一篇

邱瑞照, 李文渊, 周肃, 李廷栋, 邓晋福, 肖庆辉, 陈秀法, 元春华, 韩九曦, 王靓靓, 陈玉明, 陈正. 中国西北大陆岩石圈类型、岩石学结构及其意义[J]. 西北地质, 2008, 41(2): 1-21.
引用本文: 邱瑞照, 李文渊, 周肃, 李廷栋, 邓晋福, 肖庆辉, 陈秀法, 元春华, 韩九曦, 王靓靓, 陈玉明, 陈正. 中国西北大陆岩石圈类型、岩石学结构及其意义[J]. 西北地质, 2008, 41(2): 1-21.
shu
QIU Rui-zhao, LI Wen-yuan, ZHOU Su, LI Ting-dong, DENG Jin-fu, XIAO Qing-hui, CHEN Xiu-fa, YUAN Chun-hua, HAN Jiu-xi, WANG Liang-liang, CHEN Yu-ming, CHEN Zheng. Lithospheric Types, Petrological Structures and Their Implications in Northwestern China Continent[J]. Northwestern Geology, 2008, 41(2): 1-21.
Citation: QIU Rui-zhao, LI Wen-yuan, ZHOU Su, LI Ting-dong, DENG Jin-fu, XIAO Qing-hui, CHEN Xiu-fa, YUAN Chun-hua, HAN Jiu-xi, WANG Liang-liang, CHEN Yu-ming, CHEN Zheng. Lithospheric Types, Petrological Structures and Their Implications in Northwestern China Continent[J]. Northwestern Geology, 2008, 41(2): 1-21.
shu

中国西北大陆岩石圈类型、岩石学结构及其意义

  • 1.

    中国地质调查局发展研究中心, 北京 100037

  • 2.

    西安地质矿产研究所, 西安 710054

  • 3.

    中国地质大学, 北京 100083

  • 4.

    中国地质科学院, 北京100037

  • 5.

    中国地质大学, 北京 100083;国土资源部信息中心, 北京 100812

  • 6.

    中国地质调查局发展研究中心, 北京 100037;中国地质大学, 北京 100083

  • 基金项目: 国家科学技术部科技支撑计划课题(2006BAB01A03);国家科学技术部国际科技合作重点项目(2007DFA21380);国家自然科学基金项目(40572063);中国地质调查局项目(1212010561502,1212010711814)

Lithospheric Types, Petrological Structures and Their Implications in Northwestern China Continent

  • 1.

    Development and Research Center, China Geological Survey, Beijing 100037, China

  • 2.

    Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China

  • 3.

    China University of Geosciences, Beijing 100083, China

  • 4.

    Chinese Academy of Geological Sciences, Beijing 100037, China

  • 5.

    China University of Geosciences, Beijing 100083, China;Information Center of Ministry of Land and Resources, Beijing 100812, China

  • 6.

    Development and Research Center, China Geological Survey, Beijing 100037, China;China University of Geosciences, Beijing 100083, China

    摘要
  • 根据西北地区的地质和地球物理特征,区分出中国西北大陆以准噶尔和塔里木为代表的克拉通型岩石圈和造山带型岩石圈,而造山带型岩石圈又可以区分为以额济纳旗为代表的古生代造山带型岩石圈(老物质新结构)和包括天山、阿尔泰山、昆仑山在内的新生代造山型岩石圈(老物质新结构);依据岩石学方法、壳幔演化模型和造山带形成过程以及地震波速与岩石化学成分之间的关系,建立相应类型岩石圈的壳幔岩石学结构,讨论了不同岩石圈类型的壳幔物质结构、地壳和岩石圈地幔厚度的地质含义及其找矿意义.
    On the basis of the geological and geophysical characteristics of northw estern China continent, cratonic type and orogenic-type lithosphere represented by Junggar Basin and Tarim in northw estern China continent are distinguished. And orogenic-type lithosphere can be subdivided in to Paleozoic orogenic-type lithosphere represented by Ejinaqi (old material and new structure) and Cenozoic orogenic-type lithosphere including Tianshan Mountain, Altai and Kunlun (old material and new structure). In light of the petrologica. method, model of crust-mantle evolution, orogenic forming process, relationships between the seismic velocity and pet rochemistry composition, petrological structu reprisms corresponding with different lithospheric types have been set up, crust-mantle material structure in differen tlithospheric types, geologic meaning of crust and Mantle's thickness and its significance for prospecting have been discussed.
    • HTML全文
  • 加载中
    • 相关文章
  • 施引文献
  • 资源附件(0)
  • 加载中
计量
  • 文章访问数:  2300
  • PDF下载数:  2583
  • 施引文献:  0
出版历程
收稿日期:  2007-09-10
修回日期:  2008-01-10
刊出日期:  2008-06-15

目录

    版权所有：中国地质调查局发展研究中心 copyright @2020
    返回