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贵州海马谷地区金矿矿床特征及成矿模式
引用本文:曾昭光,杨恩林,季国松,向通.贵州海马谷地区金矿矿床特征及成矿模式[J].贵州地质,2014,31(4):261-266.
作者姓名:曾昭光  杨恩林  季国松  向通
作者单位:贵州省地矿局117地质大队,贵州贵阳,550018
摘    要:本文对海马谷地区金矿进行调查,在贵州安龙海马谷发现北东向陡倾角断层控制金矿体,其围岩为二叠系茅口组生物灰岩,矿石为硅化灰岩角砾岩。根据本次调查及收集已有勘查研究成果,建立了该区的成矿模式,认为该区北东向陡倾角断层是下一步该区重要的找矿目标。

关 键 词:贵州  海马谷  陡倾角断层  金矿特征  找矿远景

Characteristics and Metallogenic Mode of Gold Deposit in Haimagu Area of Guizhou
ZENG Zhao-guang,YANG En-lin,JI Guo-song and XIANG Tong.Characteristics and Metallogenic Mode of Gold Deposit in Haimagu Area of Guizhou[J].Guizhou Geology,2014,31(4):261-266.
Authors:ZENG Zhao-guang  YANG En-lin  JI Guo-song and XIANG Tong
Institution:117 Geological Party, Guizhou Bureau of Geology and Mineral Exploration & Development, Guiyang 550018, Guizhou, China)
Abstract:In this paper, it investigates the gold deposit in Haimagu area, NE high dip angle fauh-controlled gold deposit is found in Haimagu of Anlong, its wall-rock is biolithite limestone of Maokou formation in Pernian, the ore is silicified limestone breccia. According to this investigation and former information, the metallogenic mode is built up, it' s thought the NE high dip angle fault in this area is an important target in the next step.
Keywords:Guizhou  Haimagu  High dip angle fault  Gold deposit character  Prospecting potential
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