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湘西花垣铅锌矿田的成矿构造
引用本文:赵佳进,许明珠,刘建平,唐宇蔷,孔华,张强,杨哲.湘西花垣铅锌矿田的成矿构造[J].地质找矿论丛,2016,31(3):346-354.
作者姓名:赵佳进  许明珠  刘建平  唐宇蔷  孔华  张强  杨哲
作者单位:1. 中南大学地球科学与信息物理学院,长沙,410083;2. 四川省煤田地质局 135 队,四川 泸州,646000
基金项目:中国地质调查局“整装勘查关键基础地质研究”项目((12120114052201)资助。)
摘    要:在对湘西花垣铅锌矿田的成矿地质背景、矿床地质特征和矿石结构构造研究的基础上,重点分析了花垣矿田成矿构造特征,包括成矿前构造、成矿期构造和成矿后构造。通过矿田地质调查,认为铅锌成矿作用与液压角砾岩关系密切,而液压角砾岩为成矿期构造;根据成矿后断裂的主要特征,结合擦痕产状,反演出花垣矿田成矿后共受到3期构造应力作用;根据成矿期构造的空间分布规律(成矿期构造受花垣—张家界断裂左行走滑形成的张性空间控制)和原始礁灰岩台地的分布规律,预测了远景勘查区域。

关 键 词:花垣铅锌矿田  液压角砾岩  三大断裂  构造应力场  湘西地区
收稿时间:2015/5/14 0:00:00

The ore-forming structural of Huayuan lead-zinc ore field in western Hunan province
ZHAO Jiajin,XU Mingzhu,LIU Jianping,TANG Yuqiang,KONG Hu,ZHANG Qiang and YANG Zhe.The ore-forming structural of Huayuan lead-zinc ore field in western Hunan province[J].Contributions to Geology and Mineral Resources Research,2016,31(3):346-354.
Authors:ZHAO Jiajin  XU Mingzhu  LIU Jianping  TANG Yuqiang  KONG Hu  ZHANG Qiang and YANG Zhe
Institution:School of Geosciences and Info-physics Central South University, Changsha 410083, China;School of Geosciences and Info-physics Central South University, Changsha 410083, China;School of Geosciences and Info-physics Central South University, Changsha 410083, China;School of Geosciences and Info-physics Central South University, Changsha 410083, China;School of Geosciences and Info-physics Central South University, Changsha 410083, China;School of Geosciences and Info-physics Central South University, Changsha 410083, China;Geological Team 135 of Sichuan Coal field Geological Bureau, Luzhou 646000, Sichuan, China
Abstract:This paper briefly introduces the geological background,geological characteristics and ore tex-tures and structures of the Huayuan lead-zinc deposit in western Hunan Province and focuses on the analy-sis of characteristics of the ore-forming structure which involves the pre-mineralization structure,mineral-ization structure and post-mineralization structure.Investigation of the ore field shows that the minerali-zation is closely related to hydrofractural breccia and the breccia fracture is the syn-mineralization struc-ture.According to the characteristics of the post-mineralization fracture and the occurrence of striation the Huayuan Pb-Zn ore field are exposed to three stresses after mineralization.Prospects for further explora-tion are predicted according to spatial distribution pattern of the syn-mineralization fracture (i.e.the syn-mineralization fracture is controlled by tensional space resulted from left hand strike slip of Huayuan-Zhangjiajie fault)and reef limestone.
Keywords:Huayuan lead-zinc ore field  hydrofractural breccia  three big faults  tectonic stress field  western Hunan province
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