钾镁煌斑岩:优质金刚石主要载体与幔源流体活动标志

李睿哲, 曾普胜, 王十安, 刘斯文, 温利刚, 赵九江. 2021. 钾镁煌斑岩:优质金刚石主要载体与幔源流体活动标志[J]. 地球学报, (6): 761-770. doi: 10.3975/cagsb.2021.111001
引用本文: 李睿哲, 曾普胜, 王十安, 刘斯文, 温利刚, 赵九江. 2021. 钾镁煌斑岩:优质金刚石主要载体与幔源流体活动标志[J]. 地球学报, (6): 761-770. doi: 10.3975/cagsb.2021.111001
LI Rui-zhe, ZENG Pu-sheng, WANG Shi-an, LIU Si-wen, WEN Li-gang, ZHAO Jiu-jiang. 2021. Lamproites: The Main Carrier of High-quality Diamond and the Marker of the Activity of Mantle Source Fluids. Acta Geoscientica Sinica, (6): 761-770. doi: 10.3975/cagsb.2021.111001
Citation: LI Rui-zhe, ZENG Pu-sheng, WANG Shi-an, LIU Si-wen, WEN Li-gang, ZHAO Jiu-jiang. 2021. Lamproites: The Main Carrier of High-quality Diamond and the Marker of the Activity of Mantle Source Fluids. Acta Geoscientica Sinica, (6): 761-770. doi: 10.3975/cagsb.2021.111001

钾镁煌斑岩:优质金刚石主要载体与幔源流体活动标志

  • 基金项目:

    本文由中国地质科学院基本科研业务费项目(编号: JYYWF20180101)、山东省重点研发计划项目(公益性科技攻关类)(编号:2019GSF109101)、中国地质调查局地质调查项目(编号: DD20190589

    DD20160220

    DD20190703)和国家自然科学基金项目(编号:41072073)联合资助

详细信息
    作者简介: 李睿哲, 男, 1997年生。硕士研究生。资源与环境专业。E-mail: 13020023362@163.com
    通讯作者: 曾普胜, 男, 1964年生。博士, 教授。长期从事岩石学、矿床学、勘查地球化学研究。通讯地址: 100037, 北京市西城区百万庄大街26号。E-mail: zengpusheng@qq.com
  • 中图分类号: P542;P588.125

Lamproites: The Main Carrier of High-quality Diamond and the Marker of the Activity of Mantle Source Fluids

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    Corresponding author: ZENG Pu-sheng
  • 钾镁煌斑岩是一类较为特殊的火山成因或浅成的超基性岩, 是一种重要的深源岩石, 是深源岩浆活动的标志性产物, 可作为了解地幔信息的窗口, 也作为继金伯利岩之后的另一种金刚石寄主岩被持续关注。全球最优质的金刚石产于钾镁煌斑岩中, 主要分布于西澳阿盖尔等地。中国钾镁煌斑岩主要分布于黔湘一带、山西饮牛沟、山东大井头、湖北大洪山和西昆仑克里阳地区, 综合分析认为, 钾镁煌斑岩主要分布于深大断裂附近, 中国钾镁煌斑岩受江南台隆西缘的都匀—贵阳—铜仁—怀化深断裂、常德—安仁深断裂以及郯庐断裂带等深大断裂带控制; 贵州镇远马坪、湖南宁乡云影窝、山东平邑大井头等钾镁煌斑岩有原生金刚石产出, 钾镁煌斑岩的金刚石成矿潜力仍然有待深入研究, 尤以湘黔钾镁煌斑岩带、郯庐断裂带大井头等地可望突破。钾镁煌斑岩的标志性矿物有富钛贫铝金云母、钾碱镁闪石、镁橄榄石、镁铝榴石、铬尖晶石、铬铁矿等。其中 S1、S2组贫铝富镁铬铁矿对钾镁煌斑岩中金刚石的形成有指示意义。中国钾镁煌斑岩活动具多期性, 其中晚侏罗世—早白垩世(147—100 Ma)时期属于中国含金刚石钾镁煌斑岩和相关的金-稀土等金属矿产的重要成矿时期。
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收稿日期:  2021-08-09
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