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首页> 外文期刊>Mining & Minerals >New Ore Geology Study Findings Have Been Reported by Researchers at Tarbiat Modares University (Geology and Genesis of the North Narbaghi Cu-ag Deposit In the Urumieh-dokhtar Magmatic Arc, Iran: Fluid Inclusion and Stable Isotope Constraints)
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New Ore Geology Study Findings Have Been Reported by Researchers at Tarbiat Modares University (Geology and Genesis of the North Narbaghi Cu-ag Deposit In the Urumieh-dokhtar Magmatic Arc, Iran: Fluid Inclusion and Stable Isotope Constraints)

机译:新矿地质研究结果的报告研究Tarbiat Modares大学里(北方的地质成因Narbaghi Cu-ag存款Urumieh-dokhtar岩浆弧,伊朗:流体包裹体和稳定同位素约束)

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2022 JUL 1 (VerticalNews) – By a News Reporter-Staff News Editor at Mining & Minerals – Fresh data on Geology - Ore Geology are presented in a new report. According to news reporting originating from Tehran, Iran, by VerticalNews correspondents, research stated, “The North Narbaghi Cu-Ag deposit in the central part of the Urumieh-Dokhtar magmatic arc (UDMA) of Iran is hosted by Eocene volcanic sequences and Oligo-Miocene intrusions of arc affiliation. The mineralization can be divided into five stages that are represented by barren hydrothermal breccias, Cu-Fe sulfides cementing in the breccias, sulfosalt and sulfide hydrothermal breccias, barren post-ore quartz veinlets, and barren post-ore calcite veinlets, respectively.”
机译:2022年7月1 (VerticalNews)——由一个消息记者在采矿和矿物-新闻编辑提出了新的地质-矿石地质数据在一份新的报告。来自德黑兰,伊朗,VerticalNews记者,研究指出:“朝鲜Narbaghi Cu-Ag存款的核心部分Urumieh-Dokhtar岩浆弧(UDMA)的伊朗由始新世火山序列和Oligo-Miocene入侵弧信仰。矿化可以分为五个阶段所代表的贫瘠的热液角砾岩,Cu-Fe硫化物巩固的角砾岩,sulfosalt和硫化热液角砾岩、贫瘠的post-ore石英小静脉和贫瘠的post-ore方解石小静脉分别。”

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