吉尔吉斯斯坦北天山aktyuz - bovorrdinsky矿区金矿床中的石英-电气石交代岩

Nikolai Pak, Elena Ivleva, Vitali Shatov, Nadezhda Shatova, Anna Goncharenko
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摘要

在北天山的Aktyuz-Boordinsky矿区,发现了许多金、稀有金属和稀土金属以及贱金属的矿床和矿床。金矿床的特征是存在大量的交代岩:硅长石、钾长石、钾长石等。其中许多还具有石英-电气石质含金交代岩的特征。对石英-电气石交代岩从弱蚀变带到高蚀变带的交代带进行了矿物学和岩石学描述。石英-电气石交代岩形成脉状体和交代角砾岩,起胶结作用,碎块可由侵入岩、石英长石、钾长石和听石组成。在阿克图兹-博奥尔丁斯基矿区,石英-电气石交代岩是找矿特征,在其他地区则是找矿标志。
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Quartz-tourmaline metasomatites in gold deposits in Aktyuz-Boоrdinsky ore district (Northern Tien Shan, Kyrgyzstan)
In the Aktyuz-Boordinsky ore district in the Northern Tien Shan, numerous deposits and ore occurrences of gold, rare and rare earth metals and base metals are discovered. Gold deposits are characterized by the presence of a number of metasomatites: beresites, listvenites, K-feldspatites, etc. Many of them are also characterized by quartz-tourmaline gold-bearing metasomatites. A mineralogical and petrographic description of the metasomatic zoning of quartz-tourmaline metasomatites from weakly to highly altered zones is given. Quartz-tourmaline metasomatites form vein-like bodies and metasomatic breccias, where they act as cement, and the fragments can consist of intrusive rock, beresites, K-feldspatites, and listvenites. For the Aktyuz-Boordinsky ore district, quartz-tourmaline metasomatites are a prospecting feature for gold, and for other areas they are a prospecting criterion.
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