节点文献

福建中—新生代玄武岩的地球化学特征及其成因

Geochemical feature and genesis of the Mesozoic and Cenozoic basalt in Fujian Province

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 卢清地朱根灵秦正永

【Author】 LU Qing di 1,ZHU Gen ling 1,QIN Zheng yong 2 (1.Fujian Regional Geological Survey Party, Sanming, Fujian 365001, China; 2.Tianjin Institute of Geology and Mineral Resources, Tianjin 300170 ,China)

【机构】 福建省区域地质调查队!福建三明365001天津地质矿产研究所!天津300170

【摘要】 对福建中—新生代玄武岩的岩石化学、地球化学特征研究表明,该地区的玄武岩化学成分、微量元素和稀土元素含量都有一定的差别。这项研究对揭示源区特征和了解中国东部沿海大陆火山岩带深部地质背景提供了重要信息。

【Abstract】 The petrochemical and geochemical feature of Cenozoic basalt shows that its chemical composition and content of trace element and REE are sharply different from those of Mesozoic basalt in Fujian Province. From that, we can trace back to the difference in their characteristics of mother magma and source areas, as well as the effect of the mantle metasomatism in their evolution. The authors strive to provide some information for getting a better understanding of the background of continental volcanic rock belt located in southeastern coast of China.

  • 【文献出处】 中国区域地质 ,REGIONAL GEOLOGY OF CHINA , 编辑部邮箱 ,2000年01期
  • 【分类号】P588.145
  • 【被引频次】18
  • 【下载频次】286
节点文献中: 

本文链接的文献网络图示:

本文的引文网络