| 九瑞矿集区燕山期构造-岩浆作用及其与铜金多金属成矿关系研究 |
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| 引用本文： | 蒋少涌,徐耀明,朱志勇,周巍,孔凡斌,孙岩.九瑞矿集区燕山期构造-岩浆作用及其与铜金多金属成矿关系研究[J].岩石学报,2013,29(12):4051-4068. |
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| 作者姓名： | 蒋少涌 徐耀明 朱志勇 周巍 孔凡斌 孙岩 |
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| 作者单位： | 内生金属矿床成矿机制研究国家重点实验室, 南京大学地球科学与工程学院, 南京 210093;地质过程与矿产资源国家重点实验室, 中国地质大学, 武汉 430074;中国地质大学资源学院和紧缺战略矿产资源协同创新中心, 武汉 430074;内生金属矿床成矿机制研究国家重点实验室, 南京大学地球科学与工程学院, 南京 210093;内生金属矿床成矿机制研究国家重点实验室, 南京大学地球科学与工程学院, 南京 210093;内生金属矿床成矿机制研究国家重点实验室, 南京大学地球科学与工程学院, 南京 210093;内生金属矿床成矿机制研究国家重点实验室, 南京大学地球科学与工程学院, 南京 210093;江西省地质矿产勘查开发局赣西北大队, 九江 332000;内生金属矿床成矿机制研究国家重点实验室, 南京大学地球科学与工程学院, 南京 210093 |
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| 基金项目： | 本文受科技部973项目（2012CB416706）、十二五国家科技支撑计划（2011BAB04B03）和国家自然科学基金项目（41072055）联合资助 |
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| 摘 要： | 九瑞地区是长江中下游成矿带中最重要的铜金多金属矿集区,成矿作用可分为海西期喷流沉积期及燕山期岩浆热液期,其中燕山期的构造-岩浆热事件对成矿至关重要。本文在详细的野外矿田构造-地层-岩浆岩调查与分析及室内成岩成矿机理研究基础上,对九瑞矿集区构造系统、岩浆系统和成矿系统进行了综合研究。梳理厘定出该区主要控岩成矿断裂构造为NEE（近EW）向脆韧性走向叠掩逆冲断裂带和SN（近SN）向张扭性横向破碎断裂带。两组断裂形成“井”字形的构造格架,制约着该区的岩浆岩分布并与成矿密切相关。区内岩浆岩种类繁多,与成矿有关的主要是花岗闪长斑岩和石英闪长玢岩。两类岩体侵位的时期都集中在燕山早中期（138~148Ma）。其产状一般为岩株、岩锥、岩枝和岩墙等。岩枝、岩墙多沿NEE向逆冲断层带,尤其是沿其特有的“Y”字形断裂分布。而与成矿关系最为密切的岩株、岩锥则都侵位于NEE向和SN向断裂的交汇处。本文特别强调前人关注不够的SN（近SN）向张裂带及其控岩成矿作用。在本区确定的4组SN向张扭性带中,其中第2组宋家湾-严家村一线同NEE断裂带的几处交汇处是值得进一步详查的预测区。九瑞矿集区矿床成因类型主要包括矽卡岩型、斑岩型（包括隐爆角砾岩型）、沉积-热液叠加改造型和热液脉型等。在不同矿区,各种不同成因类型的矿床可以叠加复合为不同的矿床式,如①武山式（沉积-热液叠加改造型+矽卡岩型矿化）;②丰山洞式（矽卡岩型+隐爆角砾岩型矿化）;③城门山式（斑岩型+矽卡岩型+沉积-热液叠加改造型矿化）;④洋鸡山式（隐爆角砾岩型+斑岩型矿化）。
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| 关 键 词： | 断裂构造 断层相关褶皱 构造-岩浆带 叠加复合成矿 九瑞矿集区 |
| 收稿时间： | 2013/9/15 0:00:00 |
| 修稿时间： | 2013/11/16 0:00:00 |
Study on Mesozoic tectonics and granitic magmatism and their relationship with Cu-Au mineralization in the Jiurui ore district, Jiangxi Province |
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| JIANG ShaoYong,XU YaoMing,ZHU ZhiYong,ZHOU Wei,KONG FanBin and SUN Yan.Study on Mesozoic tectonics and granitic magmatism and their relationship with Cu-Au mineralization in the Jiurui ore district, Jiangxi Province[J].Acta Petrologica Sinica,2013,29(12):4051-4068. |
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| Authors: | JIANG ShaoYong XU YaoMing ZHU ZhiYong ZHOU Wei KONG FanBin and SUN Yan |
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| Institution: | State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China;State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China;Faculty of Earth Resources and Collaborative Innovation Center for Scarce and Strategic Mineral Resources, China University of Geosciences, Wuhan 430074;State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China;State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China;State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China;State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China;Northwestern Jiangxi Geological Team, Bureau of Exploration and Development of Geology and Mineral Researches of Jiangxi Province, Jiujiang 332000, China;State Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210093, China |
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| Abstract: | Jiurui is one of the most important Cu-Au ore district in the Lower-Middle Yangtze Valley metallogenic belt in China. There are generally two ore-forming stages in this belt, one is the Hercynian syn-sedimentary hydrothermal mineralization stage (mainly Fe-S) and the second stage is the Yanshanian magmatic-hydrothermal stage (mainly Cu-Au-Mo). Based on investigations and studies on regional structures, magmatic rocks, and various types of mineralization in the Jiurui district, we summarized the main features of structure, magmatism and mineralization in the Jiurui district. There are two main fault structures in the district that controlled the magmatic emplacement and related mineralization, namely, the strike over step thrust zones with NEE (near EW) direction and brittle-ductile character, and the transcurrent fracture fault zones with SN (near SN) direction and tonsil-torsion character. These two groups of the faults constitute a tectonic framework in the region which looks like a Chinese word "well", and they controlled the magmatic rocks and related mineralization. There are various types of magmatic rocks in this district, with the main types of grandiorite porphyry and quartz diorite-porphyry. These rocks were emplaced during the Early-Middle Yanshanian stage of 138~148Ma. These rocks display various shapes, including apophysis, harpolith, sheet, dyke, and stock. The igneous sheets and dykes are distributed along the thrust zones with NEE direction. In particular, they appear along a faulted structure with a special "Y" shape structure. But the stocks were emplaced at the cross place between the NEE direction and SN direction fault, and these rocks have a close relation with the mineralization. In this paper, we emphasized the SN direction tension faults and their controls on emplacement of granitic porphyry and related mineralization. We have identified four groups of fault with the SN direction of tonsil-torsion character in this district. We suggest that it is worth to pay more attention to the cross places between the Songjiawan-Yanjiacun line and the NEE faults for more detailed exploration. The major mineralization types in the Jiurui district include skarn type, porphyry type (including crypto-explosive breccia type), the superimposed stratabound type, and hydrothermal vein type. In a particular ore deposit, it may be a combination of various types of mineralization. For example, the Wushan deposit is a combination of skarn and superimposed stratabound ores, the Chengmenshan ore deposit is a combination of skarn, porphyry and superimposed stratabound ores. |
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| Keywords: | Fault structure Fault-related fold Tectonic-magmatic zone Superimposed mineralization Jiurui ore district |
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