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黑龙江团结沟金矿床流体包裹体研究及矿床成因
引用本文:王可勇,任云生,程新民,代军治.黑龙江团结沟金矿床流体包裹体研究及矿床成因[J].大地构造与成矿学,2004,28(2):171-178.
作者姓名:王可勇  任云生  程新民  代军治
作者单位:吉林大学,地球科学学院,吉林,长春,130061;吉林大学,地球科学学院,吉林,长春,130061;吉林大学,地球科学学院,吉林,长春,130061;吉林大学,地球科学学院,吉林,长春,130061
基金项目:吉林大学校科研和教改项目,国土资源部矿产资源定量预测及勘查评价开放实验室基金
摘    要:对团结沟金矿床赋矿岩体石英斑晶及矿石中玉髓状石英内发育的原生流体包裹体进行了系统研究 ,结果表明 ,赋矿岩体石英斑晶中主要发育含子矿物三相、气液两相、纯液相等类型包裹体 ,而矿石玉髓状石英中主要发育气液两相包裹体。测温结果显示成矿流体温度为 1 30~ 370℃ ,盐度 2~ 1 0wt%NaCl;与赋矿岩体石英斑晶中发育的气液两相包体温度、盐度范围相近 ,结合成分及氢氧同位素特征 ,认为成矿流体主要来自岩浆热液及大气降水 ,矿床成因属与中酸性斑岩侵入活动有关的中低温浅成热液金矿床

关 键 词:金矿床  流体包裹体  矿床成因  黑龙江
文章编号:1001-1552(2004)02-0171-08
修稿时间:2003年9月15日

STUDY ON FLUID INCLUSIONS OF TUANJIEGOU GOLD DEPOSIT IN HEILONGJIANG PROVINCE AND IMPLICATIONS FOR ITS GENESIS
WANG Keyong,REN Yunsheng,CHENG Xinmin and DAI Junzhi.STUDY ON FLUID INCLUSIONS OF TUANJIEGOU GOLD DEPOSIT IN HEILONGJIANG PROVINCE AND IMPLICATIONS FOR ITS GENESIS[J].Geotectonica et Metallogenia,2004,28(2):171-178.
Authors:WANG Keyong  REN Yunsheng  CHENG Xinmin and DAI Junzhi
Abstract:A systematic study on fluid inclusions developed in quartz phenocryst of ore-bearing porphyry as well as in chalcedony quartz in ores of Tuanjiegou gold deposit was carried out, the results show that daughter crystal-bearing three-phase, aqueous two-phase and pure aqueous phase etc. occur in the fluid inclusions of quartz phenocrysts from ore-bearing porphyry, while aqueous two-phase primary fluid inclusions dominate in chalcedony quartz from the ores. Microthermometric study testifies that the temperature of ore-forming solutions is between 130 and 370℃, whereas salinity varies from 2-10wt%NaCl. These values are coincident with those for aqueous two-phase fluid inclusion in quartz phenocryst. Based on the compositional analytical results of fluid inclusions, it is concluded that the ore-forming fluids mainly originated from magmatic evolution and meteoric water. The deposit is of epithermal origin related to the intrusive activities of porphyry.
Keywords:Heilongjiang  Tuanjiegou gold deposit  fluid inclusion  genesis of ore deposit
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