金矿床的变质岩及其与奥明扎陶山(克孜勒库姆中部)矿石加工的联系

IF 0.3 Q4 GEOLOGY
R. M. Sadirov, A. B. Yusupov, Sh. V. Usmanova, A. V. Tevelev
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引用次数: 0

摘要

摘要 奥明扎陶山(克孜勒库姆中部)金矿矿床的变质岩在矿物成分及其形成特征方面具有相似性,对这些变质岩进行了区分。矿石成矿的相应阶段与某些类型的变质岩有关,这些变质岩是矿石成矿的典型标志。它们反映了统一成矿系统各阶段的演变特征,可作为搜索标准。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Metasomatic Rocks of Gold Deposits and Their Connection with Ore Process of Mountain Auminzatau (Central Kyzylkum)

Metasomatic Rocks of Gold Deposits and Their Connection with Ore Process of Mountain Auminzatau (Central Kyzylkum)

Abstract

The metasomatic rocks of gold-ore deposits of the Auminzatau Mountains (Central Kyzylkum), which are similar in mineral composition and their features of the formation, are distinguished. The corresponding stages of ore mineralization are associated with certain types of metasomatic rocks, which are their typomorphic signs. They reflect the features of the evolution of the stages of a unified mineral-forming system, which can be used as search criteria.

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来源期刊
CiteScore
0.60
自引率
25.00%
发文量
43
期刊介绍: Moscow University Geology Bulletin  is the journal that mainly publishes scientific articles, short reports of graduate students, and reviews. Publications made by the members of the Faculty of Geology of the Moscow State University and their collaborators are published. Publications encompass all branches of geology.
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