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深海沉积物中的稀土矿产资源研究进展

王汾连, 何高文, 姚会强, 邓希光. 2017. 深海沉积物中的稀土矿产资源研究进展[J]. 中国地质, 44(3): 449-459. doi: 10.12029/gc20170304
引用本文: 王汾连, 何高文, 姚会强, 邓希光. 2017. 深海沉积物中的稀土矿产资源研究进展[J]. 中国地质, 44(3): 449-459. doi: 10.12029/gc20170304
WANG Fenlian, HE Gaowen, YAO Huiqiang, DENG Xiguang. 2017. The progress in the study of REE-rich deep-sea sediments[J]. Geology in China, 44(3): 449-459. doi: 10.12029/gc20170304
Citation: WANG Fenlian, HE Gaowen, YAO Huiqiang, DENG Xiguang. 2017. The progress in the study of REE-rich deep-sea sediments[J]. Geology in China, 44(3): 449-459. doi: 10.12029/gc20170304

深海沉积物中的稀土矿产资源研究进展

  • 基金项目:
    国家青年自然科学基金(41702096)、国土资源部海底矿产资源重点实验室开放基金(KLMMR-2015-A-06),中国地质调查局发展研究中心《深海沉积物稀土资源勘查规范》制定,中国科学院矿物学与成矿学重点实验室研究合作基金(KLMM20150201)资助
详细信息
    作者简介: 王汾连, 女, 1986年生, 博士, 从事大洋稀土矿产研究, E-mail:fenlian0523@163.com
    通讯作者: 姚会强, 男, 1982年生, 高级工程师, 主要从事大洋矿产资源研究, E-mail:hqyao@163.com
  • 中图分类号: P744;P618.7

The progress in the study of REE-rich deep-sea sediments

  • Fund Project: Supported by the National Natural Science Foundation of China (No. 41702096), Exoteric Foundation of MLR Key Laboratory of Marine Mineral Resources (No. KLMMR-2015-A-06), China Geological Survey Development Research Center Program (Prospecting Criterion of REE Resources in Deep-sea Sediments) and Exoteric Foundation of Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences (No. KLMM20150201)
More Information
    Author Bio: WANG Fenlian, female, born in 1986, doctor, majors in mineral deposit in the seabed; E- mail: fenlian0523@163.com .
    Corresponding author: YAO Huiqiang, male, born in 1982, senior engineer, majors in mineral deposit in the seabed; E-mail: hqyao@163.com
  • 近年发现,太平洋和印度洋的深海盆地中存在大量富含稀土的深海沉积物。主要类型为多金属软泥、沸石黏土和远洋黏土,其中的全稀土含量(∑ REY,∑ REE+Y)为400×10-6~2000×10-6,最高可达6600×10-6,重稀土含量(HREE)已达到或超过中国南方离子吸附型矿床的重稀土品位两倍以上,是潜在的新型稀土资源,具有重要的经济价值。目前不少学者对富稀土的深海沉积物进行了大量地球化学及部分矿物学的工作,认为多金属软泥中的稀土元素多赋存于与海底热液作用有关的铁锰氧化物和氢氧化物中,而沸石黏土和远洋黏土中稀土元素的富集则与磷酸盐的混入密切相关,其稀土元素主要存在于与磷灰石成分相当的生物鱼骨屑中。深海黏土的北美页岩标准化稀土配分模式与海水相似,表明其中的稀土元素主要来自于海水,REY富集成矿可能主要受控于磷灰石早期成岩阶段,期间稀土元素未发生分异。尽管近些年对深海沉积物中的稀土元素研究取得了不少成果,但是,对于沉积物中的稀土富集机制及影响因素等问题仍然需要更加深入的研究。作为稀土资源大国,为了争取我国在国际海底稀土资源竞争中的话语权,维护中国的稀土利益,中国应加紧开展相关的稀土资源勘查和潜力评价。

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  • 图 1  太平洋稀土资源分布图(据Kato Y, et al. 2011修改)

    Figure 1. 

    图 2  西太平洋富稀土深海沉积物类型

    Figure 2. 

    图 3  太平洋深海黏土中∑REY与各主量元素相关图解及CaO与P2O5相关图解

    Figure 3. 

    表 1  太平洋和印度洋不同海域深海沉积物的主量元素(%)和稀土元素含量(×10-6)特征对比

    Table 1.  The content of major elements(%) and rare earth elements(× 10-6) of the pelagic clay from the Pacific and India Ocean

    下载: 导出CSV

    表 2  西太平洋深海黏土中代表性沸石和微结核LA-ICP-MS元素分析结果

    Table 2.  Maior and Trace elemental concentrations of representative zeolite and micronodules by LA-ICP-MS

    下载: 导出CSV

    表 3  西太平洋深海粘土中鱼骨屑LA-ICP-MS元素分析结果

    Table 3.  Major and trace elemental compositions of representative fish debris by LA-ICP-MS

    下载: 导出CSV
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出版历程
收稿日期:  2017-06-03
修回日期:  2017-06-24
刊出日期:  2017-06-25

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