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甘肃北金山金矿地质特征及成矿远景浅析
引用本文:吴兴泉,李石桥.甘肃北金山金矿地质特征及成矿远景浅析[J].黄金科学技术,2014,22(3):30-35.
作者姓名:吴兴泉  李石桥
作者单位:武警黄金第十二支队,四川 成都 610036
摘    要:北金山金矿区出露地层主要有下古生界碧口群和古生界中泥盆统三河口组,其中,中泥盆统三河口组是主要的赋矿地层,与金矿关系密切。矿区断裂发育,主要有NEE、NWW和NE向3组,其中NEE向断裂控制了金矿体的产出,为主要的控矿构造。矿区岩浆活动较弱,仅见岩脉零星出露。矿区内1∶5万金、银、铜、铅、锌、砷和锑异常发育。矿区围岩蚀变主要有硅化、绢云母化和黄铁矿化,与金矿化关系密切。通过对北金山金矿地质特征和控矿因素进行系统分析,认为北金山金矿区成矿地质条件有利,具有一定的找矿前景。

关 键 词:控矿因素  地球化学特征  围岩蚀变  成矿条件  北金山金矿  甘肃省  
收稿时间:2014-01-09
修稿时间:2014-04-14

Analysis on Geological Characteristics and Metallogenic Potential of Beijinshan Gold Deposit in Gansu Province
WU Xingquan,LI Shiqiao.Analysis on Geological Characteristics and Metallogenic Potential of Beijinshan Gold Deposit in Gansu Province[J].Gold Science and Technololgy,2014,22(3):30-35.
Authors:WU Xingquan  LI Shiqiao
Affiliation:No.12 Gold Geological Party of CAPF,Chengdu   610036,Sichuan,China
Abstract:The outcropping strata of Beijinshan gold mine are mainly the Lower Paleozoic Bikou Group and the Middle Devonian Sanhekou Group.Among them,the Sanhekou Group is the main ore formation and closely retated to the gold mineralization.In mining,faults are developed which mainly have three groups of NEE,NWW and NE.NEE trending faults control the output of gold mine bodys,and also is the main ore-controlling structure. The magmatic activity in mining is weak,that only see the veins outcrop sporadically.It is abnormal development for gold,silver,copper,lead,zinc,arsenic and antimony in the gold mine.The rock alteration which have a closely related with gold mineralization mainly are silicification,sericite and pyrite,silicification,sericite and pyrite. Based on the systems analysis of geological characteristics and ore-controlling factors of the Beijinshan gold mine,it is considered to have a favorable geological condition and have a certain ore prospects,which provide a scientific basis for further exploration.
Keywords:ore-controlling factors  geochemical characteristics  wall rock alteration  mineralization condition  Beijinshan gold deposit  Gansu Province
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