大吉山花岗岩中宇宙尘的初步研究
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:


Primary Study of Cosmic Dust from Dajishan Graniite
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:

    大吉山花岗岩人工重砂中的宇宙尘呈黑色,具强磁性,平均粒径为0.206mm,按形态可分为球状、椭球状和不规则状,按成分可分为铁质和硅酸质两种类型。主要矿物有方铁矿、α-Fe、自然铜、钠长石和钾长石。主要组构类型有瘤状突起构造、喷气孔构造、“毛刺”构造、壳层构造、空腔构造、花边构造和脑纹状构造。通过研究得出如下结论:(1)大吉山宇宙尘是低氧逸度条件下高温淬火形成的非平衡结晶产物;(2)宇宙尘的来源与大吉山花岗岩的成因有密切联系,是花岗岩岩源层的残留物;(3)宇宙尘可以作为花岗岩成因指示物。

    Abstract:

    Cosmic dusts with black colour, strong magnetism and average grade of 0.206mm (from 0.1 to 0.4 mm) has been first found in the artificial pla- cers from Dajishan granite, The shapes can be divided into three groups; sphere, ellipse sphere and irregular, According to the compositions, two types, iron and silicate spherules, are distinguished, The main minerals are as follows; wustite, magnetite, a-Fe, Cu, albite and K-feldspar. The fabrics are skeleton crystal, brain-pattern, lace-Iike, pearl-string etc, Chromite, SiC and whitneyite also exist in the artificial placers, All these imply that the particles are of cos mic genesis derived from exterrestrial space, We suggest that; (1) the cosmic dus tis products of nonequilibrium crystallization under the condition of low oxy- gen fugacity, high temperature and rapid drop in temperature; ( 2 ) the source of cosmic dust has a strong relation to the genesis of Dajishan granite, the co- smic dust may be the residules of strata from which granitic magma is origi- nated; (3} cosmic dust in granite can be used as an indicator of genesis study of granitic rocks.

    参考文献
    相似文献
    引证文献
引用本文

胡雄伟,孙恭安, 1988. 大吉山花岗岩中宇宙尘的初步研究[J]. 岩石矿物学杂志, 7(3):221~227.
Hu Xiongwei Sun Gongan, 1988. Primary Study of Cosmic Dust from Dajishan Graniite[J]. Acta Petrologica et Mineralogica, 7(3): 221~227.

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