硼镁铁矿的新亚种——富锡硼镁铁矿
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 New Subspecies of Ludwigite-Tinan Ludwigite
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:

    富锡硼镁铁矿是硼镁铁矿的含锡亚种。它产于湖南常宁县七里坪镁质矽卡岩硼矿床中。矿物中SnO2变化范围为4.6—12.0%,其分子式为(Mg1.64Fe(2+(0.35))Mn(2+(0.01))(Fe(3+(0.55))Sn(0.16)Mg(0.23))BO5,这是迄今未见详细报导过的。笔者从矿物的光学物理性质、化学成分、X射线晶体学以及晶体化学等方面进行了研究。同时,与它的类似矿物在晶体学方面作了对比讨论。从以上研究中得出结论:Sn(4+)在结构中占据Fe(3+)的位置,并以伴随着的Mg(2+)作电荷补偿。还提出了Sn元素在硼镁铁矿中不仅作为微量元素存在,而且可以作为造种元素存在的新见解。

    Abstract:

    Tinan ludwigite, a new Sn-rich subspecies of ludwigite, occurs in a magnesian skarn borate deposit at Qiliping, Changning County, Hunan province. The SnO_2 content of the mineral varies from 4.6 to 12.0 wt. %, and the chemical formula is (Mg(1.64)Fe_(0.35)(2+)Mn(0.01)(2.00)(Fe(0.55)(3+)Sn(0.16)Mg(0.28))(0.99)BO5, which has never been previously reported. The authors have studied the mineral in such aspects as its optical and physical properties, chemical composition, X-ray crystallography, and crystallochemistry, with a crystallographic comparison given between this mineral and its analogues.From the above investigation, the authors have come to the conclusion that Fe(3+) position has been occupied by Sn(4+) in the crystal structure and the charge is compensated by having Mg(2+) It is also the authors' opinion that tin not only is a minor component but also serves as a species-forming element ludwigite.

    参考文献
    相似文献
    引证文献
引用本文

杨光明,潘兆橹,彭志忠, 1987. 硼镁铁矿的新亚种——富锡硼镁铁矿[J]. 岩石矿物学杂志, 6(3):229~235.
Yang Guangming, Pan Zhaolu, Peng Zhizhong, 1987. A New Subspecies of Ludwigite-Tinan Ludwigite[J]. Acta Petrologica et Mineralogica, 6(3): 229~235.

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