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滇东—黔西沉积型稀土:一种新类型稀土资源及其开发利用潜力

赖杨, 龚大兴, 秦建华, 田恩源, 惠博, 徐璐, 高泽东. 2022. 滇东—黔西沉积型稀土:一种新类型稀土资源及其开发利用潜力[J]. 中国地质, 49(6): 1823-1833. doi: 10.12029/gc20220609
引用本文: 赖杨, 龚大兴, 秦建华, 田恩源, 惠博, 徐璐, 高泽东. 2022. 滇东—黔西沉积型稀土:一种新类型稀土资源及其开发利用潜力[J]. 中国地质, 49(6): 1823-1833. doi: 10.12029/gc20220609
LAI Yang, GONG Daxing, QIN Jianhua, TIAN Enyuan, HUI Bo, XU Lu, GAO Zedong. 2022. Sedimentary rare earth in the eastern Yunnan and western Guizhou: A new genetic type and potential of development and utilization[J]. Geology in China, 49(6): 1823-1833. doi: 10.12029/gc20220609
Citation: LAI Yang, GONG Daxing, QIN Jianhua, TIAN Enyuan, HUI Bo, XU Lu, GAO Zedong. 2022. Sedimentary rare earth in the eastern Yunnan and western Guizhou: A new genetic type and potential of development and utilization[J]. Geology in China, 49(6): 1823-1833. doi: 10.12029/gc20220609

滇东—黔西沉积型稀土:一种新类型稀土资源及其开发利用潜力

  • 基金项目:
    中国地质调查局“滇黔相邻区稀土资源基地综合地质调查”项目(DD20211236)资助
详细信息
    作者简介: 赖杨, 男, 1987年生, 硕士, 工程师, 从事矿物学、区域地质矿产调查与研究工作; E-mail: 772459504@qq.com
    通讯作者: 龚大兴, 男, 1986年生, 博士, 高级工程师, 从事沉积学、区域地质矿产调查与研究工作; E-mail: 113652192@qq.com
  • 中图分类号: P618.7

Sedimentary rare earth in the eastern Yunnan and western Guizhou: A new genetic type and potential of development and utilization

  • Fund Project: Supported by the project of China Geological Survey "Comprehensive Geological Survey of Rare Earth Resource Bases in the Adjacent Areas of Yunnan and Guizhou" (No.DD20211236)
More Information
    Author Bio: LAI Yang, male, born in 1987, master, engineer, engaged in mineralogy, regional geological and mineral survey and research; E-mail: 772459504@qq.com .
    Corresponding author: GONG Daxing, male, born in 1986, Ph.D., senior engineer, engaged in sedimentology, regional geology and mineral resources survey and research work; E-mail: 113652192@qq.com
  • 研究目的

    稀土是重要的自然资源,更是宝贵且关键的战略资源。本文通过对滇东—黔西地区沉积型稀土资源野外地质调查及室内综合研究,揭示了该稀土资源的优势及开发利用潜力,既丰富了全球稀土资源工业类型,又支撑了国家关键稀土资源战略储备。

    研究方法

    本文基于对含矿地层特征、典型矿石特征、稀土元素配分特征以及稀土资源潜力等方面的研究,探讨该稀土资源的成因类型、稀土元素赋存状态以及开发利用潜力。

    研究结果

    查明含矿地层为二叠系上统宣威组(P3x);富稀土矿石的岩性为灰白色铝土质黏土岩和粉砂质黏土岩;其成因属沉积型;在威宁县黑石头—麻乍—哲觉地区,矿体厚度2~18m不等,矿体延伸较连续,稀土氧化物(TREO)含量最高达1.6%,矿体块段稀土(TREO)加权平均品位为0.18%~0.46%,推断资源量超30万t;该稀土资源中“关键稀土元素(CREE)”占比高达22.6%(以∑CREO计),高于国内外大多数正在开发利用的稀土矿;针对该稀土资源研发了“选择性浸出”新工艺,使稀土回收率达90%以上,该稀土资源有望实现规模化工业利用。

    结论

    该沉积型稀土资源具有矿体厚度大、矿石品位高、资源潜力大、开采成本低、矿石中关键稀土元素(CREO)占比高、开发利用前景好等优点。

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  • 图 1  研究区大地构造位置图(据骆耀南, 1985; 张志斌等, 2006

    Figure 1. 

    图 2  研究区地质简图

    Figure 2. 

    图 3  贵州威宁哲觉镇宣威组一段(P3x1)剖面-柱状图

    Figure 3. 

    图 4  稀土矿石扫描电镜照片

    Figure 4. 

    图 5  稀土矿找矿靶区分布图

    Figure 5. 

    图 6  全岩球粒陨石稀土配分图(据田恩源等, 2020修改;标准化数值据Sun and McDonough, 1989)

    Figure 6. 

    图 7  世界典型稀土矿床“关键稀土元素(CREE)”含量对比图(矿床序号如表 1所示)

    Figure 7. 

    图 8  稀土氧化物价格对比柱状图

    Figure 8. 

    表 1  世界典型稀土矿床对比表

    Table 1.  Comparison table of typical rare earth deposits in the world

    下载: 导出CSV
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出版历程
收稿日期:  2020-10-18
修回日期:  2021-03-14
刊出日期:  2022-12-25

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