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萤石中的杂质元素在解释矿床形成的物理化学条件时,可以用来作为成矿与岩浆岩相联系的和确定矿床相对侵蚀面及其深度等的地球化学标志,因而对它的研究具有一定的现实意义。本文的目的,在于阐明帕米尔地区萤石中杂质元素的分配特征(这些萤石是从不同成因、不同建造和不同矿物类型的形成物中挑选出来的);同时还在于确定所划分的每个组的标型元素。在所研究的地区内,我们确定了几种萤石建造类
The impurity elements in fluorite can explain the physicochemical conditions formed in the deposit and can be used as geochemical markers for the relationship between mineralization and magmatic rocks and for determining the relative erosion surface and its depth of the deposit, The practical significance. The purpose of this paper is to elucidate the distributional characteristics of the impurity elements in fluorite in the Pamir region (these fluorites were chosen from their formations of different origins, constructions, and mineral types), and also to determine the distribution of each Group of type elements. In the area under study, we identified several types of fluorite construction