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广西大厂长坡锡石硫化物矿床锡石晶胞参数的初步研究
引用本文:韩照信.广西大厂长坡锡石硫化物矿床锡石晶胞参数的初步研究[J].岩石矿物学杂志,1987,6(4):368-371.
作者姓名:韩照信
作者单位:西安地质学院
摘    要:矿床为高中温热液型锡石硫化物矿床,通过研究知道随成矿温度由高到低,成矿阶段由锡石—石英经锡右硫化物到锡石—方解石,锡石晶胞的轴长,特别是c轴长和晶胞体积都有增大趋势。锡石中含有Fe等杂质元素,它们可以类质同像代替Sn,由于这些元素离子半径小,类质同像代替结果导致晶胞变小。而在高温条件下,元素类质同像代替较易进行,这就造成了高温阶段形成的锡石晶胞小,低温阶段形成的锡石晶胞大。

关 键 词:锡石  晶胞参数  广西

A Tentative Study on Unit Cell Parameter of Cassiterite from the Changpo Cassiterite Sulphide Deposit in Dachang, Guangxi
Han Zhaoxin Xian Institute of Geology,Xian.A Tentative Study on Unit Cell Parameter of Cassiterite from the Changpo Cassiterite Sulphide Deposit in Dachang, Guangxi[J].Acta Petrologica Et Mineralogica,1987,6(4):368-371.
Authors:Han Zhaoxin Xian Institute of Geology  Xian
Abstract:The ore deposit is a hypothermal-mesothermal cassiterite sulphide one.It has been revealed through the author's investigation that with the decreasein ore-forming temperature the mineralization stages varied from cassiterite-quartz through cassiterite-sulphides to cassiterite-calcite, and cassiterite sho-wed tendency of growth both in lengths of unit cell axes, especially axis C,and in unit cell dimensions. There exist such admixture elements as Fe in cassiterite which can subs-titute isomorphously for tin. As ionic radii of these elements are usually small,the isomorphism might cause unit cell to shrink. At high temperature, isomor-phous substitution of elements takes Place rather readily, and this probablyaccounts for small unit cell of cassiterite at high temperature and larger oneat low temperature.
Keywords:cassiterite  unit cell parameter  Guangxi  
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