吉林通化赤柏松铜镍硫化物矿床Re-Os同位素研究及其地质意义

于永斌, 谢明材, 李紫源, 韩春明. 2022. 吉林通化赤柏松铜镍硫化物矿床Re-Os同位素研究及其地质意义. 地质科学, 57(1): 262-273. doi: 10.12017/dzkx.2022.016
引用本文: 于永斌, 谢明材, 李紫源, 韩春明. 2022. 吉林通化赤柏松铜镍硫化物矿床Re-Os同位素研究及其地质意义. 地质科学, 57(1): 262-273. doi: 10.12017/dzkx.2022.016
Yu Yongbin, Xie Mingcai, Li Ziyuan, Han Chunming. 2022. Re-Os isotope study and its geological significance of chibaisong Cu-Ni sulfide deposit in Tonghua, Jilin Province. Chinese Journal of Geology, 57(1): 262-273. doi: 10.12017/dzkx.2022.016
Citation: Yu Yongbin, Xie Mingcai, Li Ziyuan, Han Chunming. 2022. Re-Os isotope study and its geological significance of chibaisong Cu-Ni sulfide deposit in Tonghua, Jilin Province. Chinese Journal of Geology, 57(1): 262-273. doi: 10.12017/dzkx.2022.016

吉林通化赤柏松铜镍硫化物矿床Re-Os同位素研究及其地质意义

  • 基金项目:

    国家自然科学基金项目(编号:41772078)资助。

详细信息
    作者简介:

    于永斌,男,1965年生,教授级高级工程师,地质、矿产普查与勘探学专业。E-mail:thyuyongbin@163.com

    通讯作者: 韩春明,男,1963年生,博士,研究员,矿床学专业。本文通讯作者。E-mail:cm-han@mail.iggcas.ac.cn
  • 中图分类号: P588.12;P611

Re-Os isotope study and its geological significance of chibaisong Cu-Ni sulfide deposit in Tonghua, Jilin Province

More Information
  • 赤柏松岩浆型铜镍硫化物矿床位于华北克拉通胶辽吉带,含矿镁铁质—超镁铁质岩侵入到鞍山群最下部的四道砬子河组变质岩中;该矿床硫化物矿样品的Os和Re浓度分别为19×10-9~490×10-9和0.47×10-9~13.97×10-9,对这些数据分析得出了一条6点Re-Os等时线年龄为1 885±94 Ma,矿石的初始187Os/188Os比值为0.80±0.16(MSWD=0.17),表明矿石为岩浆源,熔体主要由地幔贡献,但在成矿过程及岩浆侵位期间有不少地壳物质混入成岩成矿系统。新的Re-Os年代学结果表明,赤柏松镁铁质—超镁铁质侵入体与铜镍矿床形成于古元古代,而不是前人认为的早白垩世。
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收稿日期:  2021-08-20
修回日期:  2021-10-20

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