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云南安宁盐矿床钙芒硝光轴角(2V)变化的初步研究

A PRELIMINARY STUDY ON THE VARIATION OF OPTICAL ANGLES (2V) OF GLAUBARITE IN A SALT DEPOSIT IN ANNING, YUNNAN PROVINCE

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【作者】 高建华; 高怀忠; 朱井泉; 韩淑静;

【Author】 Gao Jianhua Gao Huaizhong Zhu Jingquan ( Wuhan College of Geology, Wuhan 430074 )Han Shujing ( Sylvinite Division of The First Geological Team in Yunnan Province )

【机构】 武汉地质学院; 云南第一地质大队钾盐分队;

【摘要】 钙芒硝是盐类矿床中的常见矿物,光轴角小(2V=7°)一直是钙芒硝的重要鉴定特征之一。笔者研究表明:该矿床中钙芒硝的光轴角(2V)除大量为7°左右外,还有相当部分可从10°一直连续变化到接近40°。此发现对盐类矿物的鉴定具现实意义,2V变化等问题的深入研究,有助于查明盐类矿床的形成条件和沉积机理。

【Abstract】 Glauberite is a common mineral in salt deposits. Small optical angle ( 2V = 7° ) is one of the most important diagnostics for glauberite identification. We worked on a salt deposit in Anning , Yunnan 1983,and found some changes in optic angle of glauberites.The preliminary studies show that some of the glauberites have a series of optical angle changes ranging from 10* to 40*, though majority of them are 7* in this deposit. This discovery is important for identifying salt minerals. The study of the change of 2V may throw a light upon the forming conditions and recipitation mechanism of salt deposits.

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