| 陕西省陈家坝铜铅锌多金属矿床地质地球化学特征及矿床成因探讨 |
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| 引用本文： | 丁,坤.陕西省陈家坝铜铅锌多金属矿床地质地球化学特征及矿床成因探讨[J].地质与勘探,2017,53(3):436-444. |
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| 作者姓名： | 丁 坤 |
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| 作者单位： | 1. 长安大学地球科学与资源学院,陕西西安,710054;2. 长安大学地球科学与资源学院,陕西西安 710054;西北有色地质勘查局,陕西西安 710054;3. 长安大学地球科学与资源学院,陕西西安 710054;西部矿产资源与地质工程教育部重点实验室,陕西西安710054;4. 西北有色地质勘查局七一一总队,陕西汉中,723000 |
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| 基金项目： | 秦岭-大巴山-大别山成矿规律及找矿方向研究（编号：1212011220869）下设课题和西北有色地质矿业集团有限
公司博士后科研项目资助 |
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| 摘 要： | 陕西省略阳县陈家坝铜铅锌多金属矿床是"勉-略-阳"矿集区具有代表性的铜多金属矿床之一,在该矿区内已经发现了多个矿(化)体,显示出很好的成矿潜力。本文在室内外研究的基础上,详细论述了该矿床的地质和地球化学特征,采用矿床岩石主量元素、黄铁矿单矿物微量元素地球化学分析和硫同位素测试方法,对陈家坝铜铅锌多金属矿床的成矿地质特征、成矿物质来源和成矿机制进行了探讨。硫同位素特征显示,δ~(34)S主要来自海水硫酸盐,认为该矿床成矿物质主要来源于碧口岩群东沟坝组,NWW和NEE向共轭断裂是矿田内重要的控矿构造。通过黄铁矿微量元素分析显示陈家坝矿床成矿温度为中低温,成矿经历了热液作用的改造过程。综合研究认为该矿床属火山沉积-改造型矿床。
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| 关 键 词： | 铜铅锌多金属矿床 地球化学 矿床成因 勉-略-阳矿集区 陈家坝 陕西 |
| 收稿时间： | 2016/7/28 0:00:00 |
| 修稿时间： | 2017/1/5 0:00:00 |
Geochemical characteristics and ore genesis of the Chenjiaba copper-lead-zinc polymetallic deposit in Shaanxi Province |
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| Ding Kun.Geochemical characteristics and ore genesis of the Chenjiaba copper-lead-zinc polymetallic deposit in Shaanxi Province[J].Geology and Prospecting,2017,53(3):436-444. |
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| Authors: | Ding Kun |
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| Abstract: | Located in the Lueyang County of Shaanxi Province, the Chenjiaba Cu-Pb-Zn polymetallic deposit in the Mianxian-Lueyang-Yangpingguan ore concentration area is representative. A number of ore mineralization (bodies) have been found in this deposit, showing a huge metallogenic potential. Based on the laboratory study and field investigations, this paper presents detailed characteristics of geology and mineralization of this deposit. Using geochemical analysis and sulfur isotope analysis to major elements of rocks and trace elements, we explore the geological features and the source of ore-forming materials and ore-forming mechanism of the Chenjiaba Cu-Pb-Zn polymetallic deposit. The characteristics of sulfur isotopes suggest that d34S was mainly from seawater sulfate. The metallogenic matters of the deposit originated from the Donggouba Formation of the Bikou Group. The conjugate NWW- and NEE-trending faults are the major ore-controlling structure in the ore field. The analysis of trace elements in pyrite shows that the forming temperature of the Chenjiaba deposit is of middle and low values, and the mineralization has experienced the reformation process of hydrothermal fluid. The comprehensive study suggests that the deposit belongs to the volcanic sediment-reform type. |
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| Keywords: | Cu-Pb-Zn polymetallic deposit geochemistry ore genesis Mian-Lüe-Yang ore district Chenjiaba Shaanxi |
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