| 辽宁红透山铜锌矿床地质特征及成因浅析 |
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| 引用本文： | 张森, 赵东方, 吕广俊, 沙德铭, 权恒, 田昌烈, 杨铁军. 辽宁红透山铜锌矿床地质特征及成因浅析[J]. 地质与资源, 2007, 16(3): 173-182. doi: 10.13686/j.cnki.dzyzy.2007.03.006 |
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| 作者姓名： | 张森 赵东方 吕广俊 沙德铭 权恒 田昌烈 杨铁军 |
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| 作者单位： | 1.沈阳地质矿产研究所, 辽宁 沈阳 110032;; 2.辽宁省第八地质大队, 辽宁 本溪 117000;; 3.辽宁有色地勘院抚顺分院, 辽宁 抚顺 113015 |
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| 摘 要： | 红透山铜锌矿床赋存于辽北太古宙绿岩红透山岩组，为极具工业意义的大型矿床.通过对矿石H、O、S、Pb同位素特征的分析，结合矿床矿体形态、矿石结构、构造及围岩蚀变等宏观特征，认为红透山铜锌矿床成矿物质来源于太古宙晚期火山-沉积岩系，成矿流体来源于变质水和大气降水，成矿热力来源于变质作用，从而认为红透山铜锌矿床属“火山-沉积变质热液叠加”型层控矿床.
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| 关 键 词： | 红透山 铜锌矿床 地质特征 火山-沉积变质热液叠加型层控矿床 辽宁省 |
| 文章编号： | 1671-1947（2007）03-0173-10 |
| 收稿时间： | 2006-11-16 |
| 修稿时间： | 2006-11-16 |
GEOLOGY AND GENESIS OF THE HONGTOUSHAN COPPER-ZINC DEPOSIT IN LIAONING PROVINCE |
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| ZHANG Sen, ZHAO Dong-fang, LV Guang-jun, SHA De-ming, QUAN Heng, TIAN Chang-lie, YANG Tie-jun. GEOLOGY AND GENESIS OF THE HONGTOUSHAN COPPER-ZINC DEPOSIT IN LIAONING PROVINCE[J]. Geology and Resources, 2007, 16(3): 173-182. doi: 10.13686/j.cnki.dzyzy.2007.03.006 |
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| Authors: | ZHANG Sen ZHAO Dong-fang LV Guang-jun SHA De-ming QUAN Heng TIAN Chang-lie YANG Tie-jun |
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| Affiliation: | 1.Shenyang Institute of Geology and Mineral Resource, Shenyang 110032, China;; 2.Liaoning No. 8 Geologic Party, Benxi 117000, Liaonmg Province, China;; 3.Fushun Branch, Liaoning Institute of Nonferrous Geological Exploration, Fushun 113015, Liaoning Province, China |
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| Abstract: | The Hongtoushan Cu-Zn deposit,located in the Hongtoushan rock formation of Archean greenstone in North Liaoning Province,is a large-scale ore deposit with great industrial significance.According to the analysis of H,O,S and Pb isotope characteristics,accompanying with the macroscopic natures,such as the orebody shape,ore texture,structure and wall-rock alteration,it is considered that the matter source of the Hongtoushan Cu-Zn deposit is the Neoarchean volcanic-sedimentary rock series.The ore-forming fluid is originated from atmospheric water and metamorphic water.The heat for ore-forming is from metamorphism.Thus the Hongtoushan Cu-Zn deposit belongs to stratabound type with volcanic-sedimentary and metamorphic hydrothermal overprinting. |
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| Keywords: | Hongtoushan Cu-Zn deposit geologic characteristics stratabound type with volcanic-sedimentary and metamorphic hydrothermal overprinting Liaoning Province |
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