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一轴晶矿物干涉图岩组测量方法早在1939年由H·舒曼(Schumann)和1940年王嘉荫提出过。1952年山口贵雄曾对此法作过简单介绍,可是以后并沒有获得广泛的应用。 1962年我们在作变质白云岩的岩组分析时,由于白云石晶粒中发育了大量的变形页理,影响消光,于是舍弃了常用的旋转合法而改用干涉图法,效果甚好。经过多次试验证明,干涉图法对其他一轴晶矿物(如方解石、石英)也同样适用。本文就是我们通过近几年工作对干涉图法进行较系统整理的结果。干涉图法无需旋转台,这对不具备旋转台的单位开展岩组分析是一个相当有用的方法。我们认为,这对日益发展的岩组学会起一定的促进作用,同时趁此机会向同志们求正。本工作是在何作霖先生亲自指导下完成的,工作中曾得到赵宗溥先生重要的启示,在此一并志谢。
The method of measurement of the uniaxial mineralogy intergration diagram rocks was first proposed by Schumann in 1939 and Wang Jiayin in 1940. Guichi Yamaguchi 1952 had made a brief introduction to this method, but did not get a wide range of applications. In 1962 we metamorphosed dolomite rock group analysis, due to the development of a large number of dolomite deformation in the grain, the impact of extinction, then discard the rotation of the law and the use of interferograms, the effect is very good. After several tests proved that interferogram on the other uniaxial minerals (such as calcite, quartz) is also applicable. This article is the result of a more systematic review of the law of interferograms through our work in recent years. The interferogram method does not require a turntable, which is a very useful method for rock group analysis of units that do not have a turntable. In our opinion, this will play a certain catalytic role in the growing group of rock societies and will take this opportunity to seek solutions from our comrades. This work is done under the guidance of Mr. He Zuolin personally, and has been greatly inspired by Mr. Zhao Zongpu in his work.