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Geological resources of scandium: a review from a Chinese perspective

文献类型：期刊论文

作者Liu, Shang1,7,8; Fan, Hong-Rui5,6,7; Santosh, M.3,4; Liu, Xuan2; Wang, Qi-Wei7; Butcher, Alan R.2
刊名INTERNATIONAL GEOLOGY REVIEW
出版日期2023-02-01
页码22
ISSN号0020-6814
关键词Scandium deposit dispersed metal SC deposit classification SC enrichment metallogeny bayan obo deposit
DOI10.1080/00206814.2023.2169842
英文摘要Scandium (Sc) is a dispersed metal in Earth's lithosphere, with an average abundance of 16 to 22 ppm. In the meantime, it is widely considered as a critical metal because of its paramount significance in scientific research and technical innovation. With surging demands that are not backed-up by current supplies globally, the market price of Sc oxide is astonishingly five times more than the most expensive rare earth oxide of terbium (Tb). Production of Sc is significantly held back due to scarcity of economically viable grades at explorable depths within the crust, compared with other critical metals such as REE, Nb and Ta. Nevertheless, typical high- to intermediate-grade Sc deposits, as compiled in this review, consistently show close relationships to specific magmatic (e.g. ultramafic-mafic and carbonatitic), supergene and hydrothermal processes during Sc enrichment, especially the former two. Known potential Sc deposits are tentatively classified based on their host rocks and metallogeny, including those hosted in the ultramafic-mafic rocks and related laterites, in carbonatite and related laterites, in bauxite residue and processed coals, hydrothermal Sc deposits and Sc deposits related to syenite intrusions, pegmatites or marine sediments. We also discuss the Sc enrichment mechanism and associated tectonics and partition coefficients of Sc among diverse minerals and melts, which reveal the preference of Sc for clinopyroxene, garnet and iron oxides by isomorphic replacement or ion absorption during diverse magmatic and supergene Sc enrichment processes. Lastly, Sc resources in the world-class Bayan Obo deposit are discussed in detail as an illustrative benchmark example, where hydrothermal aegirine may host majority of carbonatite-derived Sc.
WOS关键词RARE-EARTH-ELEMENTS ; LA-ICP-MS ; MAFIC-ULTRAMAFIC COMPLEXES ; APATITE-MAGNETITE DEPOSIT ; TRACE-ELEMENTS ; SILICATE MELTS ; PARTITIONING COEFFICIENTS ; HEFTETJERN PEGMATITE ; CHEMICAL-COMPOSITION ; SPATIAL-DISTRIBUTION
资助项目National Natural Science Foundation of China[41902066] ; National Natural Science Foundation of China[41930430] ; Open Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization[2021Z2360] ; Joint Research Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization[2022Z2413] ; Key Research Program of Institute of Geology and Geophysics (Chinese Academy of Sciences)[IGGCAS-201901] ; Fundamental Research Funds for the Central Universities of China[lzujbky-2021-7]
WOS研究方向Geology
语种英语
出版者TAYLOR & FRANCIS INC
WOS记录号WOS:000922554500001
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Open Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Joint Research Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Joint Research Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Key Research Program of Institute of Geology and Geophysics (Chinese Academy of Sciences) ; Key Research Program of Institute of Geology and Geophysics (Chinese Academy of Sciences) ; Fundamental Research Funds for the Central Universities of China ; Fundamental Research Funds for the Central Universities of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Open Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Joint Research Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Joint Research Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Key Research Program of Institute of Geology and Geophysics (Chinese Academy of Sciences) ; Key Research Program of Institute of Geology and Geophysics (Chinese Academy of Sciences) ; Fundamental Research Funds for the Central Universities of China ; Fundamental Research Funds for the Central Universities of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Open Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Joint Research Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Joint Research Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Key Research Program of Institute of Geology and Geophysics (Chinese Academy of Sciences) ; Key Research Program of Institute of Geology and Geophysics (Chinese Academy of Sciences) ; Fundamental Research Funds for the Central Universities of China ; Fundamental Research Funds for the Central Universities of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Open Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Open Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Joint Research Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Joint Research Programme of the State Key Laboratory of Baiyunobo Rare Earth Resource Researches and Comprehensive Utilization ; Key Research Program of Institute of Geology and Geophysics (Chinese Academy of Sciences) ; Key Research Program of Institute of Geology and Geophysics (Chinese Academy of Sciences) ; Fundamental Research Funds for the Central Universities of China ; Fundamental Research Funds for the Central Universities of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/106817]  
专题地质与地球物理研究所_中国科学院矿产资源研究重点实验室
通讯作者Liu, Shang
作者单位1.Lanzhou Univ, Sch Earth Sci, Lanzhou 730000, Peoples R China
2.Geol Survey Finland, Espoo, Finland
3.Univ Adelaide, Dept Earth Sci, Adelaide, SA, Australia
4.China Univ Geosci Beijing, Sch Earth Sci & Resources, Beijing, Peoples R China
5.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Mineral Resources, Beijing, Peoples R China
7.Baotou Res Inst Rare Earths, State Key Lab Baiyunobo Rare Earth Resource Res &, Baotou, Peoples R China
8.Lanzhou Univ, Key Lab Mineral Resources Western China Gansu Prov, Lanzhou 730000, Peoples R China
推荐引用方式
GB/T 7714		 Liu, Shang,Fan, Hong-Rui,Santosh, M.,et al. Geological resources of scandium: a review from a Chinese perspective[J]. INTERNATIONAL GEOLOGY REVIEW,2023:22.
APA Liu, Shang,Fan, Hong-Rui,Santosh, M.,Liu, Xuan,Wang, Qi-Wei,&Butcher, Alan R..(2023).Geological resources of scandium: a review from a Chinese perspective.INTERNATIONAL GEOLOGY REVIEW,22.
MLA Liu, Shang,et al."Geological resources of scandium: a review from a Chinese perspective".INTERNATIONAL GEOLOGY REVIEW (2023):22.

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来源：地质与地球物理研究所

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