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大青山地区中生代玄武质火山岩岩石地球化学特征
引用本文:李晓光,李子颖,卫三元,戚大能. 大青山地区中生代玄武质火山岩岩石地球化学特征[J]. 国外铀金地质, 2009, 0(4): 202-211
作者姓名:李晓光  李子颖  卫三元  戚大能
作者单位:核工业北京地质研究院,北京100029
基金项目:致谢:本文成文过程中得到罗毅研究员、孙志富研究员、刘正义研究员的指导和夏宗强的帮助,特此致谢!
摘    要:对满洲里地区大青山盆地中生代玄武质火山岩类地球化学特征进行讨论,结合野外观察和前人资料,对其岩浆演化、成因及成岩构造环境进行探讨,为下一步工作提供依据。分析可知,该区玄武质火山岩类岩浆源于富集不相容元素的富集地幔,后有壳源物质参与,是岩石圈伸展背景下早期流体交代岩石圈地幔发生部分熔融的产物。通过火山岩地球化学特征分析以及和邻区产铀火山岩特征类比可知,本区具备较好的火山热液型铀及多金属成矿的构造环境及火山岩浆演化系列。

关 键 词:满洲里地区大青山盆地  玄武岩  岩石地球化学特征

Petrogeochemistry of Mesozoic basaltic volcanics in Daqingshan area
LI Xiao-guang,LI Zi-ying,WEI San-yuan,QI Da-neng. Petrogeochemistry of Mesozoic basaltic volcanics in Daqingshan area[J]. , 2009, 0(4): 202-211
Authors:LI Xiao-guang  LI Zi-ying  WEI San-yuan  QI Da-neng
Affiliation:(Beijing Research Institute of Uranium Geology, Beijing 100029, China)
Abstract:Through the discussion on petrogeochemistry of Later Mesozoic basaltic volcanics in Daqingshan Basin in Manzhouli area, combined with field observation and the predecessors'study, its magma evolution, genesis and diagenetic structural environment are discussed, and some suggestion are provided for the further work. Basaltic magma in this area is believed to be derived from mantle with incompatible elements which were later participated by some crustal materials. It is a partially melting product of mantle by early metasomatized fluid under lithosphere extension. Through petrogeochemical analysis of the volcanics and the contrast to the adjacent uranium-producing volcanics, it is concluded that this region has structural environment to form magma evolution series which are more favorable for volcanic hydrothermal-type uranium and polymetallic mineralization.
Keywords:Daqingshan Basin in Manzhouli area  basalt  petrogeochemical characteristics
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