栾家河花岗岩体中的矿物包裹体研究
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:


A Study of Mineral Inclusions from Luanjiahe Granite Body
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:

    根据熔融包裹体的均一温度和均一过程的时间,利用熔融包裹体的扩散率公式(DH=r2/4t)、Eyring方程(DN=KB·T/η·λ)以及不同含水量花岗质熔体的LnDH-1/T实验图解,计算了胶东金矿区内与金矿形成关系密切的栾家河岩体中包裹体熔体的粘度和含水量。结果表明,熔融包裹体均一温度为970℃,粘度为3.8×106Pa·s,含水量为2.5%;流体熔融包裹体的均一温度为855℃,粘度为617.7Pa·s,含水量为5.8%,反映出花岗岩浆在结晶过程中含水量不断增高,粘度不断降低,到结晶作用晚期,流体相接近饱和状态。

    Abstract:

    Based on homogenization temperature and duration of homogenization process obtained from Johannes (DH=r2/4t) and Eyring equations (DN=KB·T /η·λ), the authors calculated the viscosity of a melt inclusion at homogenization. The water content of the inclusion melt was estimated from the experimental diagram LnDH-1/T for granitic melt with different water contents. The study on mineral inclusions from Luanjiahe granite in Jiaodong gold zone indicates that the melt inclusion has a homogenization temperature of 970℃, viscosity of 3.8×106 Pa·s and water content of 2.5%, whereas the fluid_melt inclusion has a homogenization temperature of 855℃, viscosity of 617.7 Pa·s and water content of 5.8%, suggesting that during the crystallization of granitic magma water content increased while viscosity decreased continuously, and at the late stage of crystallization the fluid was close to the saturation state.

    参考文献
    相似文献
    引证文献
引用本文

曲晓明,王鹤年,王海芹, 1998. 栾家河花岗岩体中的矿物包裹体研究[J]. 岩石矿物学杂志, 17(3):270~274.
Qu Xiaoming, 1998. A Study of Mineral Inclusions from Luanjiahe Granite Body[J]. Acta Petrologica et Mineralogica, 17(3): 270~274.

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