地球科学进展

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2020 , Vol. 35 >Issue 5: 452 - 464

DOI: https://doi.org/10.11867/j.issn.1001-8166.2020.044

综述与评述

超深金刚石包裹体：对深部地幔物理化学环境的指示

  • 郑昕雨 ,
  • 丘志力 ,
  • 邓小芹 ,
  • 马瑛 ,
  • 陆太进
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  • 1.中山大学地球科学与工程学院 广东省地球动力作用与地质灾害重点实验室 广东省地质过程与矿产 资源探查重点实验室，广东 广州 510275
    2.自然资源部珠宝玉石首饰管理中心北京珠宝研究所 自然资源部珠宝玉石首饰检测评价创新技术中心，北京 　100013
    3.广西隐伏金属矿产勘查 重点实验室 桂林理工大学地球科学学院，广西 　桂林 　541006
郑昕雨（1995-），女，浙江丽水人，硕士研究生,主要从事宝玉石形成与重大地质事件响应研究. E-mail：zhengxy68@mail2.sysu.edu.cn

收稿日期: 2020-02-05

  修回日期: 2020-04-05

  网络出版日期: 2020-06-05

基金资助

国家自然科学基金项目“扬子克拉通深部作用过程：沅水流域砂矿大金刚石及其包裹体记录”(41473030);国家自然科学基金青年科学基金项目“黔东南与金刚石有关的石榴石精细地球化学研究”(41703028)

收起

The Inclusions in Superdeep Diamonds: Indication and Response to Deep Mantle Physical and Chemical Environment

  • Xinyu Zheng ,
  • Zhili Qiu ,
  • Xiaoqin Deng ,
  • Ying Ma ,
  • Taijin Lu
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  • 1.Guangdong Key Laboratory of Geodynamic and Geological Hazards, Guangdong Key Laboratory of Geological Process and Mineral Resources Exploration, School of Earth Science and Engineering，Sun Yat-sen University, Guangzhou 510275, China
    2.NGTC Gems＆Jewelry Institute of Beijing, Technology Innovation Center of Gems & Jewelry Inspection and Appraisal, MNR, Beijing 100013, China
    3.Guangxi Key Laboratory of Hidden Metallic Ore Deposits Exploration，College of Earth Sciences, Guilin University of Technology，Guilin Guangxi 541006, China
Zheng Xinyu （1995-）， female， Lishui City， Zhejiang Province， Master student. Research areas include gemology and mineralogy. E-mail：zhengxy68@mail2.sysu.edu.cn

Received date: 2020-02-05

  Revised date: 2020-04-05

  Online published: 2020-06-05

Supported by

the National Natural Science Foundation of China “The deep geologic process beneath the Yangtze craton: Constraints of monocrystalline diamonds from Ruan River basin and their inclusions”(41473030);“Detailed geochemistry of garnets related to the diamond in Southeastern Guizhou”(41703028)

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摘要

超深金刚石及其包裹体是探究深部地幔组成及物理化学环境的重要样本。梳理了超深金刚石中新发现的典型矿物包裹体及其组合，并结合前人高精度原位分析、高温高压合成金刚石实验的研究成果，综述分析了超深金刚石矿物包裹体及其组合指示的深度范围、微量元素与温压条件之间的关系，超深地幔水的赋存矿物相、金属相以及强还原环境新认识，残留的俯冲洋壳可能是深部地幔水的重要储库，超深金刚石及其包裹体对深俯冲及深部碳循环的指示等研究进展。指出我国学者虽然在华北、扬子克拉通金刚石中也发现了指示超深来源的矿物包裹体，在超高压金刚石形成及蛇绿岩型金刚石成因研究方面获得了某些重要进展，但对超深金刚石包裹体的研究仍然有待深入。

关键词： 超深金刚石; 包裹体; 深部地幔; 物理化学环境; 指示

本文引用格式

郑昕雨 , 丘志力 , 邓小芹 , 马瑛 , 陆太进 . 超深金刚石包裹体：对深部地幔物理化学环境的指示[J]. 地球科学进展, 2020 , 35(5) : 452 -464 . DOI: 10.11867/j.issn.1001-8166.2020.044

Abstract

Superdeep diamonds and their inclusions are important samples to probe the physical and chemical environment and constitution of Earth’s deep mantle. By combining the studies of high-precision in-situ analysis and HPHT synthetic diamond experiments, and by reviewing the new discovery of classical mineral inclusions and their combinations, the ranges of different inclusion combinations, as well as the relationship between trace elements and temperature-pressure conditions were reoriented. The so-called nominally anhydrous minerals combinations, metal phases and redox environments in superdeep mantle were also affirmed. Meanwhile，the recent findings of inclusions and isotopes in superdeep diamonds support the fact that the remaining subduction ocean crust may be a significant reservoir of the deep mantle’s water and the deep mantle carbon cycle is closely related to oceanic subduction. Furthermore, although Chinese scholars have discovered some kinds of superdeep inclusions in diamonds from North China Craton and Yangtze Craton, and made considerable progress in the study of the formation of UHP diamonds and the genesis of ophiolite diamonds, there are still many scientific questions about superdeep diamonds that require further research.

Key words： Superdeep diamond; Inclusions; Deep mantle; Physicochemical environment; Indication and response

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