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贵州晴隆大厂锑矿地质及控矿因素
引用本文:刁理品,韩润生,刘鸿,李波,王雷.贵州晴隆大厂锑矿地质及控矿因素[J].云南地质,2006,25(4):467-473.
作者姓名:刁理品  韩润生  刘鸿  李波  王雷
作者单位:1. 昆明理工大学国土资源工程学院,有色金属矿产地质调查中心西南地质调查所,云南,昆明,650093
2. 贵州晴隆大厂锑矿,贵州,晴隆,561409
基金项目:国家财政部资补项目;教育部跨世纪优秀人才培养计划
摘    要:大厂锑矿田主要控矿因素有地层、岩性、玄武岩、构造及古岩溶面特征等;“大厂层”是为主要含矿层位,而古岩溶面控制了“大厂层”的产出特征;构造控制了矿床、矿体的分布;玄武岩与成矿作用有成因联系。

关 键 词:"大厂层"  构造  控矿因素  大厂锑矿田  晴隆  贵州
文章编号:1004-1885(2006)04-

Study on geology and ore-controlling factors In Qinglong Dachang Antimony Orefield of Guizhou Province
DIAO Li-pin,HAN Run-sheng,LIU Hong,LI Bo,WANG Lei.Study on geology and ore-controlling factors In Qinglong Dachang Antimony Orefield of Guizhou Province[J].Yunnan Geology,2006,25(4):467-473.
Authors:DIAO Li-pin  HAN Run-sheng  LIU Hong  LI Bo  WANG Lei
Institution:1. Faculty of Land and Resources Engineering, Kunming University of Science and Technology; Southwest Institute of Geological Survey, Geological Survey Center for Non -ferrous Mineral Resources, Kunming 650093 ; 2. Qinglong Antimony Mine, Qinglong, Guizhou 561409
Abstract:Dachang Antimony Orefield is mainly controlled by stratum,lithological character,basalt,structure and physiognomy of the ancient dissolved-rock.The "Dachang layer" is the major ore-bearing layer.physiognomy of the ancient dissolved-rock controls the output of the "Dachang layer".Different deposits are controlled by various Structures.Basalt has relationship with ore-form process.
Keywords:"Dachang layer"  ore-controlling factors  structure  Dachang Antimony Orefield  Guizhou
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