| 湘西大脑坡矿区沉积-断裂构造特征及其对铅锌成矿控制作用 |
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| 引用本文： | 刘敏,毛党龙,周旭林,周皓迪.湘西大脑坡矿区沉积-断裂构造特征及其对铅锌成矿控制作用[J].西北地质,2022(1):129-141. |
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| 作者姓名： | 刘敏 毛党龙 周旭林 周皓迪 |
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| 作者单位： | 湖南省国土资源规划院;湖南地科院规划设计有限公司;国土资源评价与利用湖南省重点实验室;湖南省矿产资源储量评审中心 |
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| 基金项目： | 湖南省矿产资源储量评审中心国家矿产资源储量技术标准体系建设项目之子课题“重要有色金属与贵金属及稀土稀有矿床合理勘查程度研究”(CB2015-2-5)资助。 |
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| 摘 要： | 为了明确大脑坡矿区沉积和断裂构造特征,以及沉积和断裂构造对铅锌成矿控制作用,笔者从大脑坡矿区沉积-断裂构造特征出发,识别了大脑坡矿区生物礁沉积,并进一步将大脑坡矿区主要断裂系统划分为3个断裂带,即花垣-张家界断裂带(F1为主断层)、阿碧林场-清水塘断裂带(F2为主断层)、开支铺-凉水井断裂带(F3为主断层).通过分析断...
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| 关 键 词： | 大脑坡矿区 沉积 断裂 断裂系统 控矿模式 有利区 |
Tectonic Features of Deposition and Faults of Danaopo Mining Area in Western Hunan and the Controlling Effect on Pb-Zn Mineralization |
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| LIU Min,MAO Danglong,ZHOU Xulin,ZHOU Haodi.Tectonic Features of Deposition and Faults of Danaopo Mining Area in Western Hunan and the Controlling Effect on Pb-Zn Mineralization[J].Northwestern Geology,2022(1):129-141. |
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| Authors: | LIU Min MAO Danglong ZHOU Xulin ZHOU Haodi |
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| Institution: | (Hunan Provincial Land and Resources Planning Institute, Changsha 410114, Hunan, China;Hunan Academy of Geosciences Planning and Design Co., Ltd., Changsha 410114, Hunan, China;Hunan Provincial Key Laboratory of Land Resources Evaluation and Utilization, Changsha 410114, Hunan, China;The Mineral Resources and Resources Evaluation Center of Hunan, Changsha 410114, Hunan, China) |
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| Abstract: | In order to clarify the tectonic features of deposition and faults in Danaopo mining area and the controlling effect on the Pb-Zn mineralization,this paper identified the reef deposits of this area and divided the main fault systems into three fault systems:Huayuan-Zhangjiajie fault zone(F1 main fault),Abilinchang-Qingshuitang fault zone(F2 main fault)and Kaizhipu-Liangshuijing fault zone(F3 main fault)Layer.The fault systems are further divided into three types based on the relationship between the stages of fault activity and mineralization:regional inherited fault,metallogenic fault and post metallogenic fault.The regional inherited fault is mainly Huayuan-Zhangjiajie fault;the fault in the metallogenic period is mainly F2,F108 and F2-1 faults in Abilinchang-Qingshuitang.The distribution of the post metallogenic fault,which develops in the whole area,is more complicated because of the post metallogenic tectonic stress.Based on the relationship between the sedimentary environment,the fracture structure and the mineralization of Qingxudong Formation in Danaopo mining area,it is considered that the main metallogenic model is that when the deep ore fluid moves upward in the metallogenic period by the algal limestone through the regional inherited faults,the metallogenic fluid in the ideal space undergoes metasomatism and deposition,forming the mineralization.The authors thus summarize the metallogenic law of lead-zinc deposits in Danaopo mining area and believe that the regional inherited large fault(Huayuan-Zhangjiajie fault zone)controls the extension and distribution of the whole ore field.The joints and the secondary faults in the metallogenic period is the concentrating area of high-grade ore body. |
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| Keywords: | Danaopo mining area deposition fault fault system ore controlling model favorable mineralization area |
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