Abstract

The sulfur isotope composition was measured in the main morphological types and generations of sulfides composing the ores of the Dzhusa deposit and the contents of trace elements were measured using highly sensitive laser ablation-inductively coupled plasma-mass spectrometry (LA–ICP–MS) for the first time. According to the sulfur isotope geochemistry, we assume that a deep magmatic source made a predominant contribution to the ore-forming fluid. Using the STATISTICA software modules, correlation analysis was performed and the trace element distribution patterns in sulfides were revealed.

中文翻译：

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卓萨硫铁矿-多金属矿床的矿石的同位素组成和地球化学特征（南乌拉尔）

摘要

用高灵敏度的激光烧蚀-电感耦合等离子体质谱法（LA-ICP-MS）测量了构成Dzhusa矿床矿石的主要形态类型和硫化物世代的硫同位素组成，并测量了痕量元素的含量。第一次。根据硫同位素地球化学，我们假设深部岩浆源对成矿流体做出了主要贡献。使用STATISTICA软件模块进行了相关分析，并揭示了硫化物中的痕量元素分布模式。