| 注册
首页|期刊导航|岩矿测试|湖南鲁塘石墨矿Re-Os同位素研究

湖南鲁塘石墨矿Re-Os同位素研究

李超 王登红 周利敏 赵鸿 李欣尉 屈文俊

岩矿测试2017,Vol.36Issue(3):297-304,8.
岩矿测试2017,Vol.36Issue(3):297-304,8.DOI:10.15898/j.cnki.11-2131/td.201704060050

湖南鲁塘石墨矿Re-Os同位素研究

Study on the Re-Os Isotope Composition of Graphite from the Lutang Graphite Deposit in Hunan Province

李超 1王登红 2周利敏 3赵鸿 1李欣尉 3屈文俊3

作者信息

  • 1. 中国地质科学院矿产资源研究所,北京100037
  • 2. 北京大学造山带与地壳演化教育部重点实验室,北京100871
  • 3. 国家地质实验测试中心,北京100037
  • 折叠

摘要

Abstract

Graphite has relatively high Re and Os contents and is an ideal mineral for Re-Os isotope dating.However,there are few studies on Re-Os dating of graphite.Particularly for the graphite which was formed by deformation of coal beds,the variation in Re-Os isotope system needs further study.The Lutang graphite deposit in Hunan is one of the typical cryptocrystalline graphite deposits in China.The orebodies are hosted in coals of the Permian Longtan Formation.In this study,the Re-Os isotopic compositions of the graphite samples from Lutang deposit and the raw coal samples from the peripheral area were analyzed by digesting sample in the Carius tube,direct distilling Os from the Carius tube,extracting Re by acetone and determining Re and Os isotopes by Negtive Thermal Ionization Mass Spectrometry.The results indicate that the Re and Os contents are 0.901-9.794 ng/g and 7.3-189.5 pg/g,respectively.The Re-Os isotope isochron age is 155.6 ±3.6 Ma,which is consistent with the zircon U-Pb age (153-157 Ma) of Stage Ⅱ medium-grained biotite granite of the Qitianling pluton on the east side of the deposit.It also indicates that the coal seam of the Longtan Formation is subjected to ‘baking’ by the Qitianling pluton,inducing the hot contact metamorphism and changing the raw coal near the Qitianling pluton to graphite to form a graphite deposit.The comparison of Re and Os content and Os isotopic composition between the graphite,coal and Qitianlign pluton demonstrates that the Re and Os in the graphite are mainly derived from raw coal.According to the initial Os isotope ratio of 0.686 ± 0.032,it can be concluded that minor Os with low 187Os/188Os value was absorbed by carbonaceous material during the intrusion of coal seam by the Qitianling pluton.

关键词

鲁塘/石墨矿/成因/Re-Os同位素/定年

Key words

Lu tang/graphite deposit/genesis/Re-Os isotope/dating

分类

天文与地球科学

引用本文复制引用

李超,王登红,周利敏,赵鸿,李欣尉,屈文俊..湖南鲁塘石墨矿Re-Os同位素研究[J].岩矿测试,2017,36(3):297-304,8.

基金项目

国家自然科学基金面上项目(41673060) (41673060)

中国地质调查局地质调查项目(DD20160095) (DD20160095)

岩矿测试

OA北大核心CSCDCSTPCD

0254-5357

访问量3
|
下载量0
段落导航相关论文