| 豫西熊耳山地区吉家洼金矿床成矿物质来源探讨——碳、氧、硫、铅同位素地球化学证据 |
| Received:February 25, 2016 Revised:April 16, 2017 点此下载全文 |
| 引用本文：ZHANG XingKang,YE HuiShou,ZHANG Wei,ZHANG FuBin,HE XuQi,ZHANG XiangCun.2017.C, O, S and Pb isotopic constraints on ore-forming material sources of Jijiawa gold deposit in Xiong'er Mountain area, western Henan[J].Mineral Deposits,36(3):595~610 |
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| Author Name | Affiliation | E-mail | | ZHANG XingKang | Hebei Institute of Geological Survey, Shijiazhuang, 050081, Hebei, China
MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | | | YE HuiShou | MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China | yehuishou@163.com | | ZHANG Wei | Hebei Institute of Geological Survey, Shijiazhuang, 050081, Hebei, China | | | ZHANG FuBin | Hebei Institute of Geological Survey, Shijiazhuang, 050081, Hebei, China | | | HE XuQi | The Fourth Geological Exploration Institute, Henan Bureau of Geology and Mineral Resources, Zhengzhou 450001, Henan, China | | | ZHANG XiangCun | No.3 Institute of Geological & Mineral Resources Survey, Henan Bureau of Geology and Mineral Resources, Zhengzhou 450003, Henan, China | |
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| 基金项目:本文得到中国地质调查局地质调查项目（编号：1212011220869）和国土资源部成矿作用与资源评价重点实验室开放研究项目（编号：ZS1314）的联合资助 |
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| 中文摘要:吉家洼金矿床位于豫西熊耳山金多金属矿集区中西部，矿体产出受断裂构造控制，属构造蚀变岩-石英脉型金矿床。为了查明吉家洼金矿床的成矿物质来源，本次对矿床的碳、氧、硫、铅等同位素进行了系统研究。研究结果表明，吉家洼金矿的δ13CV-PDB介于-10.3‰~-7.7‰之间，δ18OV-SMOW介于14.2‰~17.8‰之间，表明成矿流体中的碳来源于岩浆。硫化物δ34S值介于-20.4‰~-5.4‰，表明硫来源于早白垩世花山花岗岩基，造成硫化物的δ34S值呈现出较大负值的原因可能是在成矿过程中成矿流体物理化学条件的变化引起硫同位素发生分馏所致。铅同位素组成为206Pb/204Pb=17.042~18.149，207Pb/204Pb=15.333~15.575，208Pb/204Pb=37.675~38.868，与由新太古界-古元古界太华群岩石重熔形成的早白垩世花岗岩的铅同位素组成相似，具有壳幔混合源的特点。综合碳、氧、硫、铅等同位素的研究结果认为，吉家洼金矿床的成矿流体来源于岩浆热液，并有大气降水的加入；成矿物质主要来源于早白垩世花岗岩，矿床成因属岩浆期后热液脉状金矿床。 |
| 中文关键词:地球化学 碳、氧、硫、铅同位素 成矿物质来源 吉家洼金矿 熊耳山地区 |
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| C, O, S and Pb isotopic constraints on ore-forming material sources of Jijiawa gold deposit in Xiong'er Mountain area, western Henan |
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| Abstract:The Jijiawa gold deposit is located in the western part of the Xiong'er Mountain gold polymetallic ore concentration area, Henan Province. The formation of orebodies was controlled by the subsidiary fault which was located in the faulted structure belt. Based on systematic field study of isotopes such as C, O, S and Pb, the authors focused on the source of ore-forming materials. With the δ13CV-PDB values ranging from -10.3‰ to -7.7‰ and the δ18OV-SMOW ranging from 14.2‰ to 17.8‰, the C-O isotopes composition reveals that C isotope originated in magmatic-dominated fluid. The δ34S values vary from -20.4‰ to -5.4‰, suggesting that S isotope originated in early Cretaceous Huashan granite. In the process of mineralization, the change of physico-chemical conditions led to sulfur isotope fractionation, which is probably the reason that the δ34S presents a large negative value. The 206Pb/204Pb ratios are 17.042~18.149, 207Pb/204Pb ratios are 15.333~15.575 and 208Pb/204Pb ratios are 37.675~38.868, suggesting that Pb has a characteristic of crust-mantle mixed source, and it is similar to Early cretaceous granites in lead isotope composition. Based on the study of C, O, S, Pb isotopes, the authors consider that the hydrothermal system was gradually transitional from a magmatic-dominated fluid to a meteoric-dominated fluid, and early Cretaceous granite contributed main metallogenic materials. The Jijiawa Au gold deposit genetically belongs to magmatic hydrothermal vein gold deposit. |
| keywords:geochemistry C-O-S-Pb isotopes source of ore-forming material Jijiawa Au deposit Xiong'er Mountain area |
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