确定南澜沧江缝合带的火山岩地球化学证据
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:


Geochemical Evidence of Volcanic Rocks for Determining the South Lancangjiang Suture Zone
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    本文着重根据火山岩的主量元素、稀土元素和微量元素特征厘定了我国西南“三江”地区昌宁-孟连带C1—P2火山岩和南澜沧江带P—T3火山岩的构造-岩浆类型。昌宁-孟连火山岩带为洋脊/准洋脊型-洋岛型玄武岩、蛇绿混杂岩带,代表澜沧江洋或古特提斯的残迹;南澜沧江火山岩带是一个陆缘火山弧带,是澜沧江洋盆向东俯冲消减、碰撞以及陆内俯冲过程的产物。两带火山岩是成对分布的古特提斯缝合带的产物。

    Abstract:

    The present paper deals with volcanic rocks of the Changning-Menglian belt (C1-P 2) and the south Lancangjiang belt (P1-T3) in "Sanjiang" region, Southwest China. Based On geological and petrological characteristics of these volcanic rocks, the authors studied their major elements, REE and trace element and, furthermore, determined their tectonomagmatic types. Volcanic rocks along the Changning-Menglian belt are basalts and ophiolite complex of oceanic ridge paraoceanic ridge type, which represent remnants of the Lancangjiang ocean. The South Lancangjiang volcanic belt is a composite volcanic arc resulting from eastward subducting and collision of the Lancangjiang ocean. The two volcanic belts, distributed in pairs, are products of the Lancangjiang oceanic suture zone.

    参考文献
    相似文献
    引证文献
引用本文

朱勤文,张双全,谭 劲, 1998. 确定南澜沧江缝合带的火山岩地球化学证据[J]. 岩石矿物学杂志, 17(4):296~307.
Zhu Qinwen Zhang Shuangquan Tan Jin, 1998. Geochemical Evidence of Volcanic Rocks for Determining the South Lancangjiang Suture Zone[J]. Acta Petrologica et Mineralogica, 17(4): 296~307.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:
  • 最后修改日期:
  • 录用日期:
  • 在线发布日期:
  • 出版日期:
文章二维码