普里皮亚季含钾盆地钾盐矿的微组构特征

N. S. Petrova, N. Denisova, Aliaksei V. Kirykovich
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引用次数: 2

摘要

普里皮亚季含钾盆地对复杂底土使用的要求越来越高:新技术类型的钾盐矿,有用成分含量较低,有害杂质浓度增加。利用各种复杂的质量指标对自然类型钾盐矿进行评价无疑是钾盐矿床特点的优先考虑因素。自Starobin矿床发现以来,对钾盐矿床的结构、结构特征和组成的研究一直受到重视。Starobin矿床发现后,开始了对盐岩岩石学的系统研究。到目前为止,在岩石学中,还没有公认的钾盐(钾镁)矿盐岩结构的合理成因分类。某些结构的名称是基于表现明亮的次生特征、颜色或与不同物体的相似性。本工作的目的是对岩石的初级沉积特征进行元素识别,根据石化参数对初级和次级特征进行系统化和类型化。本文介绍了普里皮亚季盆地红色和斑点状高盐组合矿床的典型钾盐矿的主要微构造类型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Microfabric characteristics of potash ore of the Pripyat potash-bearing basin
The requirements of complex subsoil use are increasing in the Pripyat potash-bearing basin: potash ore of new technologic types, with lower contents of useful components, increased concentrations of harmful impurities. Using all complex of quality indicators assessment of natural types of potash ore is undoubtedly prioritized by characteristic of potash deposits. The study of structural and textural features and composition of potash deposits has been given attention since the time of discover of the Starobin deposit. Systematic study of salt rock petrology has been started after the discovery of the Starobin deposit. Until now in the petrology, there is no recognized rational genetic classification of the structures of salt rocks being potash (potassium-magnesium) ore. The name of certain structure is based on the secondary features that are brightly expressed, color or similarity with different objects. The aim of the present work is an element recognition of the primary sedimentary features of rocks, systematization of primary and secondary characteristics and their typification according to petrochemical parameters. In the article the main microfabric types of potash ore that are typical for the deposits of red-colored and mottled hypersaline association of the Pripyat basin.
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