Localization patterns of gold mineralization in the Phuoc Son area, Central Vietnam

T. Tran Van, P. Ignatov, T. Mai Trong
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Abstract

Background. In this paper, the authors aim to reveal the localization patterns of gold mineralization in the Phuok Son region of Central Vietnam, which formed a Proterozoic-Cambrian metamorphic complex in the zone of the Late Paleozoic Benzhang–Queshon granite block.Aim. To determine the localization patterns of gold mineralization in the Phuoc Son area, Central Vietnam.Materials and methods. The research was based on geological materials, as well as mine working and appraisal well data. The material composition of the materials was studied using 15 transparent sections and 18 polished sections. In total, 127 samples were subjected to atomic absorption spectroscopy.Results. Within the Phuoс Son gold ore field in Central Vietnam, the site of the Baidat and Baigo mines located in the zone of reverse-shear termination was investigated. Here, the gold ore bodies are represented by quartz-sulfide veins subparallel to schistosity. The ore-bearing zones are layered zones of tectonic faults, which formed at the end of the reverse-shear period and complicated the western limbs and locks of the anticlines. These zones were formed under regional sublatitudinal horizontal stresses. The horizons of carbonaceous quartz-sericite schists are of great importance in ore control. There are steeply dipping post-ore faults that displace ore bodies. Two gold mineralization stages can be distinguished. The early stage was characterized by a wide development of sphalerite and a smaller amount of gold. The later stage was associated with the main precipitation of gold and formation of galena. According to the geochronological data on the argon isotopy in biotite, the gold mineralization at Baidat and Baigo was probably formed in the Triassic (250–200 Ma ago), at the stage of extinction of the regional metamorphism of the Indosinian orogenyConclusion. The results obtained should be used when conducting local forecasting of gold deposits in Central Vietnam.
越南中部福山地区金矿化的定位模式
背景。本文旨在揭示在晚古生代本章—曲顺花岗岩块体带形成元古宙—寒武系变质杂岩的越南中部Phuok Son地区金矿化的定位模式。目的:确定越南中部福山地区金矿化的定位模式。材料和方法。研究以地质资料、矿山工作及评价井资料为基础。采用15个透明截面和18个抛光截面研究了材料的材料组成。共对127个样品进行了原子吸收光谱分析。在越南中部phuovinson金矿田内,对位于反剪切终止带的Baidat和Baigo矿址进行了调查。此处的金矿体以与片岩近平行的石英硫化物脉体为代表。含矿带为层状构造断裂带,形成于逆剪切末期,使背斜西支、西锁更为复杂。这些带是在区域次向水平应力作用下形成的。碳质石英绢云母片岩的层位对控矿具有重要意义。有陡倾的后矿断层置换矿体。可区分两个金矿化阶段。早期闪锌矿广泛发育,金含量较少。后期与金的主要沉淀和方铅矿的形成有关。根据黑云母中氩同位素的年代学资料,认为拜达特和白戈的金矿化可能形成于三叠纪(250 ~ 200 Ma),处于印支造山期区域变质作用的灭绝阶段。所得结果可用于越南中部地区金矿床的局部预测。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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