Volume 32 Issue 5
Oct.  2026
Turn off MathJax
Article Contents
WANG R C,2026. Mineral systems, evolutionary patterns, and spatial mineral prospecting methods for rare-metal mineralization[J]. Journal of Geomechanics,32(5):1150−1161 doi: 10.12090/j.issn.1006-6616.2026133
Citation: WANG R C,2026. Mineral systems, evolutionary patterns, and spatial mineral prospecting methods for rare-metal mineralization[J]. Journal of Geomechanics,32(5):1150−1161 doi: 10.12090/j.issn.1006-6616.2026133

Mineral systems, evolutionary patterns, and spatial mineral prospecting methods for rare-metal mineralization

doi: 10.12090/j.issn.1006-6616.2026133
Funds:  This research was financially supported by the National Natural Science Foundation of China (Grant Nos. 42230809 and 92462302).
More Information
  • Author Bio:

    王汝成,南京大学教授,国家杰出青年科学基金获得者,2025年获第十九次李四光地质科学奖科研奖。长期从事稀有金属矿物学和成矿理论研究,聚焦矿物晶体化学理论,破解稀有金属矿物“稀、细、伴”的系列研究难题,构建稀有金属“元素富集—矿物承载—矿床形成”研究体系。获国家自然科学奖二等奖1项、教育部自然科学奖一等奖2项等。担任中国矿物岩石地球化学学会副理事长、国务院学位委员会地质学科评议组成员兼秘书长

  • Received: 2026-09-09
  • Revised: 2026-09-17
  • Accepted: 2026-09-23
  • Available Online: 2026-09-29
  • Published: 2026-10-28
  •   Objective  Rare metals are an important subset of critical strategic metals, and their mineralization is closely related to the granite–pegmatite system. As direct products of mineralization, the crystallization behavior and evolutionary patterns of rare-metal minerals provide an essential basis for understanding metallogenic mechanisms, assessing resource potential, and predicting ore-forming districts.   Methods  A systematic analysis of rare-metal minerals in different geological and metallogenic settings has been carried out.   Results  This study identifies (hydro)oxides, silicates, and phosphates as the main types of rare-metal ore minerals and systematically analyzes their mineralogical characteristics. At the global scale, it investigates the evolutionary features of these minerals during key geological periods, revealing the relationship between rare-metal mineralization and supercontinent assembly–breakup cycles. Based on differences in element electronegativity, it establishes the relationship between the chemical behavior of rare elements and their mineralization potential, elucidating the fundamental processes of rare-metal enrichment and mineralization. At the orebody scale, it systematically analyzes the crystallization sequence of lithium minerals and develops a generalized evolutionary framework for lithium mineralization in rare-metal pegmatites. Furthermore, from the perspective of compositional evolution in Nb–Ta and Zr–Hf minerals, it develops a multi-dimensional tracing system for rare-metal mineralization.   Conclusions  This study establishes a comprehensive mineral system for rare-metal mineralization and develops a mineral-centered mineralization processes, thereby advancing our understanding of the evolutionary patterns of rare-metal mineralization.  Significance  This work will promote the establishment of a spatial prospecting methodology based on mineralogical responses and offer theoretical support for rare-metal resource exploration.

     

  • Full-text Translaiton by iFLYTEK

    The full translation of the current issue may be delayed. If you encounter a 404 page, please try again later.
  • loading
  • [1]
    ČERNÝ P, 1991. Rare-element granitic pegmatites. Part I: anatomy and internal evolution of pegmatitic deposits[J]. Geoscience Canada, 18(2): 49-67.
    [2]
    CORREIA NEVES J M, LOPES NUNES J E L, SAHAMA T G, 1974. High hafnium members of the zircon-hafnon series from the granite pegmatites of Zambézia, Mozambique[J]. Contributions to Mineralogy and Petrology, 48(1): 73-80. doi: 10.1007/BF00399111
    [3]
    ENGHAG P. 2004. Encyclopedia of the Elements: Technical Data-History-Processing-Applications. WILEY-VCH Verlag GmbH & Co. KGaA,Weinheim, Online ISBN:9783527612338.
    [4]
    EVENSEN J M, LONDON D, 2002. Experimental silicate mineral/melt partition coefficients for beryllium and the crustal Be cycle from migmatite to pegmatite[J]. Geochimica et Cosmochimica Acta, 66(12): 2239-2265. doi: 10.1016/S0016-7037(02)00889-X
    [5]
    GOLDSCHMIDT V M, 1937. The principles of distribution of chemical elements in minerals and rocks. The seventh Hugo Müller Lecture, delivered before the Chemical Society on March 17th, 1937[J]. Journal of the Chemical Society, 140: 655-673. doi: 10.1039/jr9370000655
    [6]
    GREW E S, BOSI F, ROS L, et al., 2018. Fluor-elbaite, lepidolite and Ta–Nb oxides from a pegmatite of the 3000 Ma Sinceni Pluton, Swaziland: evidence for lithium–cesium–tantalum (LCT) pegmatites in the Mesoarchean[J]. European Journal of Mineralogy, 30(2): 205-218. doi: 10.1127/ejm/2017/0029-2686
    [7]
    GUO C J, WANG Z G, 1981. The evolution of minerals[J]. Acta Mineralogica Sinica(1): 1-9. (in Chinese with English abstract)
    [8]
    HOU Z Q, CHEN J, ZHAI M G, 2020. Current status and frontiers of research on critical mineral resources[J]. Chinese Science Bulletin, 65(33): 3651-3652. (in Chinese with English abstract) doi: 10.1360/tb-2020-1417
    [9]
    HU F Y, LIU X C, HE S X, et al., 2023. Cesium-rubidium mineralization in Himalayan leucogranites[J]. Science China Earth Sciences, 66(12): 2827-2852. doi: 10.1007/s11430-022-1159-3
    [10]
    HUANG X L, WANG R C, CHEN X M, et al., 2002. Vertical variations in the mineralogy of the Yichun topaz-lepidolite granite, Jiangxi Province, southern China[J]. The Canadian Mineralogist, 40(4): 1047-1068. doi: 10.2113/gscanmin.40.4.1047
    [11]
    LEE C T, 2016. Geochemical classification of elements[M]//WHITE W M. Encyclopedia of geochemistry: a comprehensive reference source on the chemistry of the earth. Cham: Springer: 545-549, doi: 10.1007/978-3-319-39312-4_255.
    [12]
    LINNEN R L, KEPPLER H, 1997. Columbite solubility in granitic melts: consequences for the enrichment and fractionation of Nb and Ta in the Earth’s crust[J]. Contributions to Mineralogy and Petrology, 128(2): 213-227. doi: 10.1007/s004100050304
    [13]
    LINNEN R L, CUNEY M, 2005. Granite-related rare-element deposits and experimental constraints on Ta-Nb-W-Sn-Zr-Hf mineralization[M]//LINNEN R L, SAMSON I M. Rare-element geochemistry and mineral deposits. St. John's: Geological Association of Canada: 1745-1768.
    [14]
    LIU C, WANG R C, XIE L, et al., 2020. Spodumene pegmatites from the Pusila pluton in the Higher Himalaya, South Tibet: Lithium mineralization in a highly fractionated leucogranite batholith[J]. Lithos, 258-259: 105421
    [15]
    LONDON D, MORGAN VI G B, ICENHOWER J, 1998. Stability and solubility of pollucite in the granite system at 200 MPa H2O[J]. The Canadian Mineralogist, 36(2): 497-510. doi: 10.3749/canmin.er00001
    [16]
    MANETA V, BAKER D R, MINARIK W, 2015. Evidence for lithium-aluminosilicate supersaturation of pegmatite-forming melts[J]. Contributions to Mineralogy and Petrology, 170(1): 4. doi: 10.1007/s00410-015-1158-z
    [17]
    MARIGNAC C, CUNEY M, 1999. Ore deposits of the French Massif Central: insight into the metallogenesis of the Variscan collision belt[J]. Mineralium Deposita, 34(5): 472-504. doi: 10.1007/s001260050216
    [18]
    MCCAULEY A, BRADLEY D C, 2014. The global age distribution of granitic pegmatites[J]. The Canadian Mineralogist, 52(2): 183-190. doi: 10.3749/canmin.52.2.183
    [19]
    MCNEIL A G, LINNEN R L, FLEMMING R L, et al., 2020. An experimental approach to examine fluid-melt interaction and mineralization in rare-metal pegmatites[J]. American Mineralogist, 105(7): 1078-1087. doi: 10.2138/am-2020-7216
    [20]
    ROMER R L, KRONER U, 2016. Phanerozoic tin and tungsten mineralization: tectonic controls on the distribution of enriched protoliths and heat sources for crustal melting[J]. Gondwana Research, 31: 60-95. doi: 10.1016/j.gr.2015.11.002
    [21]
    RUDNICK R L, GAO S, 2014. Composition of the continental crust[M]//HOLLAND H D, TUREKIAN K K. Treatise on geochemistry. 2nd ed. Amsterdam: Elsevier: 1-51.
    [22]
    SCHWARTZ M O, RAJAH S S, ASKURY A K, et al., 1995. The Southeast Asian tin belt[J]. Earth-Science Reviews, 38(2-4): 95-293. doi: 10.1016/0012-8252(95)00004-T
    [23]
    SONG Y, DONG S C, HU H, et al., 2023. Global temporospatial distribution patterns of Nb/Ta-bearing minerals based on big data analytics[J]. Earth Science Frontiers, 30(5): 197-204. (in Chinese with English abstract)
    [24]
    STILLING A, ĆERNÝ P, VANSTONE P J, 2006. The Tanco pegmatite at Bernic Lake, Manitoba. XVI. Zonal and bulk compositions and their petrogenetic significance[J]. The Canadian Mineralogist, 44(3): 599-623. doi: 10.2113/gscanmin.44.3.599
    [25]
    TANG Y, ZHANG H, RAO B, 2016. The effect of phosphorus on manganocolumbite and mangaotantalite solubility in peralkaline to peraluminous granitic melts[J]. American Mineralogist, 101(2): 415-422. doi: 10.2138/am-2016-5424
    [26]
    TKACHEV A V, 2011. Evolution of metallogeny of granitic pegmatites associated with orogens throughout geological time[M]//SIAL A N, BETTENCOURT J S, DE CAMPOS C P, et al. Granite-related ore deposits. London: Geological Society of London: 7-23.
    [27]
    VAN LICHTERVELDE M, HOLTZ F, DZIONY W, et al., 2011. Incorporation mechanisms of Ta and Nb in zircon and implications for pegmatitic systems[J]. American Mineralogist, 96(7): 1079-1089. doi: 10.2138/am.2011.3650
    [28]
    VON KNORRING O, HORNUNG G, 1961. Hafnian zircons[J]. Nature, 190(4781): 1098-1099. doi: 10.1038/1901098a0
    [29]
    WANG R C, CHE X D, XIE L, et al., 2026. Deciphering the regional distribution patterns, petrogenetic types, and metallogenic systems of rare-metal granites in South China[J]. Science China Earth Sciences, 69(9): 3197-3211. doi: 10.1007/s11430-025-1990-4
    [30]
    WANG R C, HU H, ZHANG A C, et al., 2007. Cs-dominant polylithionite in the Koktokay#3 pegmatite, Altai, NW China: in situ micro-characterization and implication for the storage of radioactive cesium[J]. Contributions to Mineralogy and Petrology, 153(3): 355-367. doi: 10.1007/s00410-006-0151-y
    [31]
    WANG R C, WU F Y, XIE L, et al., 2017. A preliminary study of rare-metal mineralization in the Himalayan leucogranite belts, South Tibet[J]. Science China Earth Sciences, 60(9): 1655-1663. doi: 10.1007/s11430-017-9075-8
    [32]
    WANG X J, ZOU T R, XU J G, et al. , 1981. Study of pegmatite minerals from the Altai region[M]. Beijing: Scientific Publishing House: 140. (in Chinese)
    [33]
    WATSON E B, HARRISON T M, 1983. Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types[J]. Earth and Planetary Science Letters, 64(2): 295-304. doi: 10.1016/0012-821X(83)90211-X
    [34]
    WU F Y, LIU X C, HU F Y, et al., 2024. Himalayan leucogranites: rare-metal resources[J]. Elements, 20(6): 401-408. doi: 10.2138/gselements.20.6.401
    [35]
    XU K X, XIE L, WANG R C, et al., 2025. Mineralogical characteristics of the Lhozhag pegmatites in the Himalaya orogen and the occurrence state and enrichment process of cesium within the pegmatites[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 44(6): 1301-1318. (in Chinese with English abstract) doi: 10.3724/j.issn.1007-2802.20250082
    [36]
    XU Z H, WANG R C, XIE L, et al., 2026. Rb-Cs mineralization of Chaya in the Mount Qomolangma region, Himalaya[J]. Acta Petrologica Sinica, 42(5): 1715-1734. (in Chinese with English abstract)
    [37]
    YANG Y P, ZHANG Y X, SIMON A, et al., 2016. Cassiterite dissolution and Sn diffusion in silicate melts of variable water content[J]. Chemical Geology, 441: 162-176. doi: 10.1016/j.chemgeo.2016.07.021
    [38]
    YANG Z Y, WANG R C, CHE X D, et al., 2022. Paragenesis of Li minerals in the Nanyangshan rare-metal pegmatite, Northern China: toward a generalized sequence of Li crystallization in Li-Cs-Ta-type granitic pegmatites[J]. American Mineralogist, 107(12): 2155-2166. doi: 10.2138/am-2022-8285
    [39]
    YIN R, WANG R C, ZHANG A C, et al., 2013. Extreme fractionation from zircon to hafnon in the Koktokay No. 1 granitic pegmatite, Altai, northwestern China[J]. American Mineralogist, 98(10): 1714-1724. doi: 10.2138/am.2013.4494
    [40]
    ZHANG Y M, 1975. Metasomatic processes and Ta-Nb mineralization characteristics in a granitic pegmatite in a mining area of Henan Province[M]//Proceedings of national rare-element geology conference. Beijing: Geological Publishing House: 218-228. (in Chinese)
    [41]
    ZHAO Y M, FENG C Y, LI D X, et al., 2017. Li, Be-bearing ribbon rocks and related metasomatites in Xianghualing tin-polymetallic deposit, Hunan Province[J]. Mineral Deposits, 36(6): 1245-1262. (in Chinese with English abstract)
    [42]
    郭承基, 王中刚, 1981. 矿物演化[J]. 矿物学报(1): 1-9.
    [43]
    侯增谦, 陈骏, 翟明国, 2020. 战略性关键矿产研究现状与科学前沿[J]. 科学通报, 65(33): 3651-3652. doi: 10.1360/TB-2020-1417
    [44]
    胡方泱, 刘小驰, 何少雄, 等, 2023. 喜马拉雅淡色花岗岩铷铯成矿作用[J]. 中国科学: 地球科学, 53(12): 2868-2895.
    [45]
    宋颜, 董少春, 胡欢, 等, 2023. 基于大数据的铌钽矿物全球时空分布特征分析[J]. 地学前缘, 30(5): 197-204. doi: 10.13745/j.esf.sf.2023.5.12
    [46]
    王汝成, 吴福元, 谢磊, 等, 2017. 藏南喜马拉雅淡色花岗岩稀有金属成矿作用初步研究[J]. 中国科学: 地球科学, 47(8): 871-880. doi: 10.1360/N072017-00036
    [47]
    王汝成, 车旭东, 谢磊, 等, 2026. 华南稀有金属花岗岩的区域分带、类型划分和成矿系统[J]. 中国科学: 地球科学, 56(9): 3243-3257. doi: 10.1360/SSTE-2025-0448
    [48]
    王贤觉, 邹天人, 徐建国, 等, 1981. 阿尔泰伟晶岩矿物研究[M]. 北京: 科学出版社: 140.
    [49]
    徐渴鑫, 谢磊, 王汝成, 等, 2025. 喜马拉雅洛扎伟晶岩矿物学特征及铯赋存状态与富集过程[J]. 矿物岩石地球化学通报, 44(6): 1301-1318. doi: 10.3724/j.issn.1007-2802.20250082
    [50]
    徐志豪, 王汝成, 谢磊, 等, 2026. 喜马拉雅珠峰地区查雅山铷铯成矿作用[J]. 岩石学报, 42(5): 1715-1734. doi: 10.18654/1000-0569/2026.05.09
    [51]
    张玉铭, 1975. 河南某矿区花岗伟晶岩的交代作用和钽铌矿化特征[M]//全国稀有元素地质会议论文汇编小组. 全国稀有元素地质会议论文集(第二集). 北京: 地质出版社: 218-228.
    [52]
    赵一鸣, 丰成友, 李大新, 等, 2017. 湖南香花岭锡铍多金属矿区的含Li、Be条纹岩和有关交代岩[J]. 矿床地质, 36(6): 1245-1262. doi: 10.16111/j.0258-7106.2017.06.001
  • 加载中

Catalog

    Figures(6)  / Tables(3)

    Article Metrics

    Article views (103) PDF downloads(17) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return