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贵州天柱磨山—油麻坳金矿化带岩石矿物地球化学研究
引用本文:张杰,余大龙,张先煜,杨勇俊.贵州天柱磨山—油麻坳金矿化带岩石矿物地球化学研究[J].地质与勘探,1998(2).
作者姓名:张杰  余大龙  张先煜  杨勇俊
作者单位:贵州工业大学资源工程系
摘    要:研究了贵州天柱磨山—油麻坳金矿化带的成矿条件、控矿规律及地球化学特征。认为:金元素来源于地层;成矿流体具变质水和大气降水混合特征;褶皱翼部与断裂交汇带及层间破碎带等控制着矿体产出。成矿作用过程具沉积变质改造作用特点,多期次的构造变质作用对金元素的迁移聚集有着重要控制作用。

关 键 词:金矿化带  脉型金矿  金矿地球化学  贵州天柱

PETROLOGICAL,MINERALOGICAL AND GEOCHEMICAL STUDY OF THE MOSHAN-YOUMAAO GOLD MINERALIZED ZONE IN GUIZHOU PROVINCE
Zhang jie,Yu dalong,Zhang xianyu,Yan yongjun.PETROLOGICAL,MINERALOGICAL AND GEOCHEMICAL STUDY OF THE MOSHAN-YOUMAAO GOLD MINERALIZED ZONE IN GUIZHOU PROVINCE[J].Geology and Prospecting,1998(2).
Authors:Zhang jie  Yu dalong  Zhang xianyu  Yan yongjun
Abstract:The gold-bearing quartz vein of the Mosmaa-Youmaao mineralized zone in Tianzhu Guizhou province occurs in the Qingshuijiang formation of the Xiajiang group volcanic tuffaceous slate. Orefluids were mainly derived from mixing flow of the meteoric water and metamorphic water.Metalloginic environment was the weak reduction type.It is obvious that the initial stage,the tectonics movement and hydrothermal reformation took place the gold element in rich in strata,in the late stage,the gold-bearing quartz veins have been reached through repeated concentration of such metallogenic element as gold under the action of multiple geologic and fluid reforming processes.
Keywords:gold mineralized zone  vein-gold deposit  gold deposit geochemistry  Tianzhu  Guizhou  
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