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碳酸岩型稀土矿床成矿流体演化机制研究现状及展望

李胜虎, 于学峰, 田京祥, 单伟, 沈昆. 2021. 碳酸岩型稀土矿床成矿流体演化机制研究现状及展望[J]. 中国地质, 48(2): 447-459. doi: 10.12029/gc20210207
引用本文: 李胜虎, 于学峰, 田京祥, 单伟, 沈昆. 2021. 碳酸岩型稀土矿床成矿流体演化机制研究现状及展望[J]. 中国地质, 48(2): 447-459. doi: 10.12029/gc20210207
LI Shenghu, YU Xuefeng, TIAN Jingxiang, SHAN Wei, SHEN Kun. 2021. Research status and prospect of the evolution mechanism of ore-forming fluids for carbonatite-hosted REE deposits[J]. Geology in China, 48(2): 447-459. doi: 10.12029/gc20210207
Citation: LI Shenghu, YU Xuefeng, TIAN Jingxiang, SHAN Wei, SHEN Kun. 2021. Research status and prospect of the evolution mechanism of ore-forming fluids for carbonatite-hosted REE deposits[J]. Geology in China, 48(2): 447-459. doi: 10.12029/gc20210207

碳酸岩型稀土矿床成矿流体演化机制研究现状及展望

  • 基金项目:
    山东省自然科学基金青年项目(ZR2020QD029、ZR2019PD019)、山东省博士后创新项目专项资金(201903084)和山东地质勘查基金(鲁勘字(2019)8号、鲁勘字(2020)7号)联合资助
详细信息
    作者简介: 李胜虎, 男, 1985年生, 博士, 主要从事成矿流体高温高压实验模拟研究; E-mail: lshcugb@163.com
  • 中图分类号: P618.7

Research status and prospect of the evolution mechanism of ore-forming fluids for carbonatite-hosted REE deposits

  • Fund Project: Supported by Shandong Provincial Natural Science Foundation Youth Project (No.ZR2020QD029, No. ZR2019PD019), Shandong Postdoctoral Innovation Project Special Fund (No.201903084) and Geological Exploration Project of Shandong Province (No. Lukanzi (2019) 8, No.Lukanzi (2020) 7)
More Information
    Author Bio: LI Shenghu, male, born in 1985, doctor, engaged in high temperature and high pressure experimental simulation of ore-forming fluids; E-mail: lshcugb@163.com .
  • 与碱性岩有关的碳酸岩型内生稀土矿床在中国乃至世界上轻稀土资源储量中占有极为重要的地位,诸如我国内蒙古的白云鄂博稀土矿床、川西冕宁—德昌稀土成矿带中的牦牛坪、大陆槽等稀土矿床、山东微山县郗山稀土矿床以及美国的Mountain Pass稀土矿床等都属于这种类型的稀土矿床。当前,对于这类稀土矿床的成矿流体演化机制,学界主要存在结晶分异作用、不混溶作用(熔体-熔体不混溶、熔体-流体不混溶以及流体-流体不混溶)以及热液交代蚀变作用之间的分歧。结晶分异作用可以使具有不相容性的稀土元素在残余熔体相中逐渐富集,直至形成稀土矿物。不混溶作用能够使稀土元素在不混溶后形成的两相或多相中的某一相中发生选择性富集,形成稀土矿化。成矿流体演化晚阶段的热液流体对早期生成的矿物或围岩进行交代蚀变,使其释放出能与稀土元素在热液中形成络合物的F-、(CO3)2-以及(SO4)2-等阴离子(团),并最终在合适的构造控矿部位和外界环境条件下,重结晶或沉淀出稀土矿物。上述3种观点各有其理论依据,但是在解释一些碳酸岩型稀土矿床地质现象或实验地球化学模拟结果的时候都或多或少存在一定程度上的不足。前人的研究结果表明,碳酸岩型稀土矿床中发育了大量的熔体包裹体、熔体-流体包裹体以及富CO2的流体包裹体,以往在利用Linkam TS1400XY以及Linkam THMS600等这类常规高温热台,在101325 Pa条件下对其进行热力学测温时,这些包裹体大多在尚未达到完全均一状态前就已发生爆裂或泄露,极大制约了人们对这类稀土矿床在高温岩浆阶段和中高温岩浆-热液阶段成矿流体演化过程的认知。另外,对于稀土元素在成矿流体演化过程中的含量变化特征及其地球化学行为的研究,目前主要是通过包裹体成分组成的拉曼光谱分析,以及对矿体和围岩进行的全岩地球化学分析,尚缺乏单个包裹体中元素含量的原位微区分析方面的数据。未来,对碳酸岩型稀土矿床中发育的熔体包裹体、熔体-流体包裹体和富CO2的流体包裹体,利用热液金刚石压腔开展高温高压原位均一实验模拟研究,以及对单个包裹体中微量元素的含量利用LA-ICP-MS进行原位微区分析,将是揭示该类稀土矿床成矿流体演化机制的关键。

  • 加载中
  • 图 1  上地幔橄榄岩低度部分熔融形成的初始岩浆在结晶分异作用下REE进行富集的模型(据Cullers and Medaris, 1977)

    Figure 1. 

    图 2  碱土、碱性元素在碳酸盐-硅酸盐不混溶熔体间的分配系数

    Figure 2. 

    图 3  REE在共生的碳酸盐-硅酸盐两相中的分配系数

    Figure 3. 

    图 4  Kalkfeld碳酸岩及其出溶盐流体中REE和其他微量元素的含量(据Bühn and Rankin, 1999)

    Figure 4. 

    图 5  牦牛坪REE矿床成矿流体演化P-T轨迹示意图(据Xie et al., 2009)

    Figure 5. 

    图 6  深源岩浆在缓慢冷却和结晶过程中发生的两相碳酸盐-硅酸盐熔体不混溶以及多相碳酸盐-盐类熔体不混溶过程示意图(据Panina and Motorina, 2008修改)

    Figure 6. 

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出版历程
收稿日期:  2020-07-10
修回日期:  2021-02-25
刊出日期:  2021-04-25

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