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矿物流体包裹体中稀有气体的保存能力初探
引用本文:张东亮,郑德顺,彭建堂,袁顺达.矿物流体包裹体中稀有气体的保存能力初探[J].矿床地质,2011,30(5):933-940.
作者姓名:张东亮  郑德顺  彭建堂  袁顺达
作者单位:1. 中南大学有色金属成矿预测教育部重点实验室,地球科学与信息物理学院,湖南长沙410083
2. 河南理工大学资源环境学院,河南焦作,454000
3. 中南大学有色金属成矿预测教育部重点实验室,地球科学与信息物理学院,湖南长沙410083;中国科学院地球化学研究所矿床地球化学国家重点实验室,贵州贵阳550002
4. 中国地质科学院矿产资源研究所,北京,100037
基金项目:本文得到国家自然科学基金项目(编号:40902033;41073036)和中南大学青年教师助推基金(编号:201012200125)资助
摘    要:查明流体包裹体中稀有气体的保存能力,对于判断其初始组分特征是否因后生作用而发生改变具有重要意义.文章以Ar为例,从扩散动力学角度对稀有气体地球化学研究中常用的矿物中流体包裹体稀有气体的保存能力进行了定量分析和系统比较,计算了Ar在这些矿物中的封闭温度以及不同温度条件下的保存时间,得出相同条件下各矿物对Ar、He等保存能...

关 键 词:地球化学  流体包裹体  矿物  稀有气体  保存能力

A preliminary study of the retention of noble gases in fluid inclusions of different minerals
ZHANG DongLiang,ZHENG DeShun,PENG JianTang,YUAN ShunDa.A preliminary study of the retention of noble gases in fluid inclusions of different minerals[J].Mineral Deposits,2011,30(5):933-940.
Authors:ZHANG DongLiang  ZHENG DeShun  PENG JianTang  YUAN ShunDa
Institution:ZHANG DongLiang1,ZHENG DeShun2,PENG JianTang1,3 and YUAN ShunDa4(1 Key Laboratory of Metallogenic Prediction of Nonferrous Metals,Ministry of Education,School of Geosciences and Info-physics,Central South University,Changsha 410083,Hunan,China,2 Institute of Resources and Environment,Henan Polytechnic University,Jiaozuo 454000,Henan,3 State Key Laboratory of Ore Deposit Geochemistry,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,Guizhou,4 Institute of Mineral Resources,Chin...
Abstract:Studies of the retention of noble gases in fluid inclusions from various hydrothermal minerals are necessary for tracing the source of ore-forming fluid by using noble gas isotopic geochemistry. Mainly with Ar as an example, the retention of noble gases in several minerals commonly used to study fluid inclusion geochemistry was quantitatively evaluated and systematically compared with each other in this paper in terms of diffusion dynamics. In addition, closure temperature and preservation time of noble gases in these minerals were also calculated. The result reveals that, under the same conditions, the component characteristics of Ar, He and other noble gases can be preserved in these minerals in order of barite (=celestite) > chalcopyrite > pyrite > galena > sylvite > sphalerite > fluorite > wolframite > scheelite > beryl > calcite > quartz. It is also indicated that the closure temperature of Ar in quartz is more sensitive to the change of grain size than that of other minerals and will increase rapidly with the radius of the crystal, but the diffusivity is insensitive to the change of temperature. On such a basis, the authors present a theoretical scale for accurate assessment of variations of noble gas components resulting from post-entrapment processes.
Keywords:geochemistry  fluid inclusions  mineral  noble gases  retention
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