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八卦庙金矿床中含金石英脉的地球化学特征及意义
引用本文:郑作平,于学元.八卦庙金矿床中含金石英脉的地球化学特征及意义[J].岩石矿物学杂志,1996,15(4):339-345.
作者姓名:郑作平  于学元
作者单位:中国科学院广州地球化学研究所
摘    要:八卦庙金矿床是分布于秦岭造山带中的一种中高温碳酸盐型热液金矿床。石英是其主要的脉石矿物之一,与金矿化密切相关。根据含金石英脉的产状可将其分为三种类型:①顺层石英脉;②含铁白云石石英脉;③NE向节理石英脉。它们在微量元素和稀土元素的组成特征上有一定的差异,分别形成于金的不同成矿阶段,是金在成矿作用过程中演化的产物。同时,为八卦庙金矿的成矿提供了条件。石英中包裹体测温结果为八卦庙金矿床的中温成因提供了证据

关 键 词:含金石英脉  地球化学  八卦庙金矿床  秦岭

Geochemistry of Auriferous Quartz Veins in the Baguamiao Gold Deposit
Zheng Zuoping,Yu Xueyuan.Geochemistry of Auriferous Quartz Veins in the Baguamiao Gold Deposit[J].Acta Petrologica Et Mineralogica,1996,15(4):339-345.
Authors:Zheng Zuoping  Yu Xueyuan
Abstract:The Baguamiao gold deposit in a sort of mesothermal hypothermal carbonate type gold deposit. Quartz, one of the major gangue minerals, is closely related to gold mineralization. According to modes of occurrence, auriferous quartz veins might be divided into three types:(1) bedding quartz veins;(2) ferriferous dolomite quartz veins;(3)quartz veins along NE trending joints. These types show certain differences in compositional characteristics of trace elements and rare earth elements and were formed respectively at different ore forming stages of gold, being evolutional products of gold in the process of ore forming process. Thermometric measurements of inclusions in quartz have provided evidence for mesothermal hypothermal origin of the Baguamiao gold deposit.
Keywords:auriferous quartz vein  geochemistry  Baguamiao gold deposit  Qinling
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