佩特里科夫钾盐矿床凝灰岩层位的结构和矿物学组成

Zhurnal Belorusskogo gosudarstvennogo universiteta Geografiia geologiia Pub Date : 2019-06-27 DOI:10.33581/2521-6740-2019-1-119-127

V. P. Samodurov, Anatoly I. Druk, K. Balashov, Yuriy N. Yalenski

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引用次数: 1

摘要

本文介绍了北谢斯托维奇向斜带上泥盆统地层标志凝灰岩层的结构和矿物学组成的综合资料。揭示了凝灰岩层结构与火山活动阶段的关系。发现凝灰岩的主导矿物为构造有序的伊利石1M。显着凝灰岩层位位于Petrikov向斜带的上泥盆统盐层内，向上进入周围地质层的上覆泥灰岩组。

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Structure and mineralogical composition of the tuff horizon of Petrikov potash deposit

Integrated data of the structure and mineralogical composition of the marking tuff horizon in the Upper-Devonian bed of the North-Shestovich synclinal zone are presented in this paper. Dependence of the tuff bed structure on the volcanic activity stage is revealed. Find out that the prevailing mineral of tuff is the structure-ordered illite 1M. Marked tuff horizon is situated inside the Upper-Devonian salt bed within Petrikov synclinal zone and comes up into the overlaying clay-marl formation of the surrounding geological beds.

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来源期刊

Zhurnal Belorusskogo gosudarstvennogo universiteta Geografiia geologiia

自引率

0.00%

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审稿时长

12 weeks