中国矿物岩石地球化学学会第18届侯德封矿物岩石地球化学青年科学家奖经过初审函评后，于2020年10月10日在上海召开了评审会。经侯德封奖评选工作委员会预审和综合评议，最后以无记名投票方式评选出20名获奖人。 

　　根据《侯德封奖实施办法》，评选结果在提交本会常务理事会通讯审议后进行了为期10天的公示（公示时间：2020年10月23日至2020年11月1日），现公示期满，评选结果生效。现公告如下（以分组姓氏汉语拼音排序）。 　　

矿 物 学 组

　　李 艳，女，1982年2月生，北京大学地球与空间科学学院副教授、博士 

　　请奖项目：天然半导体矿物光电转化效应 

　　与请奖项目有关的主要学术成就与创新点：①发现地表普遍发育铁锰氧化物“矿物膜”转化太阳能效应，揭示地表非生物光电转化作用利用太阳能新途径，为地表过程利用太阳能提供新认识与新证据。②发现半导体矿物光电子能量促进非光合微生物生长代谢，揭示日光—无机矿物—有机生物复杂界面上光子—光电子—价电子能量传递与转化基本过程，丰富了对矿物与微生物交互作用方式的认识。③建立原位、微区测定天然矿物半导体光电特性新方法，系统揭示地表半导体矿物缺陷态赋予的可见光催化作用机制，拓展了地表多种电子能量形式作用下锰循环过程的认知。 

　　五篇代表性论著： 

　　1.Anhuai Lu#, Yan Li#, Hongrui Ding, Xiaoming Xu, Yanzhang Li, Guiping Ren, Jing Liang, Yuwei Liu, Hao Hong, Ning Chen, Shengqi Chu, Feifei Liu, Yan Li, Haoran Wang, Cong Ding, Changqiu Wang, Yong Lai, Juan Liu, Jeffrey Dick, Kaihui Liu, Michael F. Hochella Jr.. Photoelectric conversion on Earth’s surface via widespread Fe- and Mn-mineral coatings. Proceedings of the National Academy of Sciences of the United States of America. 2019, www.pnas.org/cgi/doi/10.1073/pnas.1902473116. 

　　2. Anhuai Lu#, Yan Li#, Song Jin, Xin Wang, Xiaolei Wu, Cuiping Zeng, Yan Li, Hongrui Ding, Ruixia Hao, Ming Lv, Changqiu Wang, Yueqin Tang, Hailiang Dong. Growth of non-phototrophic microorganisms using solar energy through mineral photocatalysis. Nature Communications. 2012, 3: 768-775.  

　　3.Yan Li, Feifei Liu, Xiaoming Xu, Yuwei Liu, Yanzhang Li, Hongrui Ding, Ning Chen, Hui Yin, He Lin, Changqiu Wang, Anhuai Lu. Influence of heavy metal sorption pathway on the structure of biogenic birnessite: Insight from the band structure and photostability. Geochimica et Cosmochimica Acta. 2019, 256: 116-134. 

　　4.Yan Li, Xiao Wang, Jianshu Duan, Hongrui Ding, Yanzhang Li, Anhuai Lu, Changqiu Wang, Yong Nie, Xiaolei Wu. Coupled anaerobic and aerobic microbial processes for Mn-carbonate precipitation: A realistic model of inorganic carbon pool formation. Geochimica et Cosmochimica Acta. 2019, 256: 49-65. 

　　5.Yanzhang Li, Yan Li*, Xiaoming Xu, Cong Ding, Ning Chen, Hongrui Ding, Anhuai Lu. Structural disorder controlled oxygen vacancy and photocatalytic activity of spinel-type minerals: A case study of ZnFe2O4. Chemical Geology. 2019, 504: 276-287. 

　　  

　　刘 冬，男，1981年1月生，中国科学院广州地球化学研究所特任研究员，博士 

　　请奖项目：硅藻土中主要矿物的界面作用机制及其生物地球化学效应  

　　与请奖项目有关的主要学术成就与创新点：在硅藻蛋白石和粘土矿物等硅藻土的主要组成矿物的微结构和表界面反应性上取得了新认识，包括：①发现和揭示了硅藻生物成因蛋白石结构中铝的来源和赋存机制，提出硅藻生物硅是全球重要铝汇，阐释了相关的硅-铝-碳共循环机制；②发现了硅藻蛋白石表面金属氧化物膜的存在，更新了对硅藻蛋白石矿物和硅藻土矿石性质的认识；③提出了基于同一探针分子分析矿物表面固体酸性的新方法，阐释了硅藻蛋白石和主要粘土矿物的表面固体酸性及其效应和机理。 

　　五篇代表性论著： 

　　1. Liu, D.; Yuan, P.; Tian, Q.; Liu, H.; Deng, L.; Song, Y.; Zhou, J.; Losic, D.; Zhou, J.; Song, H., Lake sedimentary biogenic silica from diatoms constitutes a significant global sink for aluminium. Nature Communications. 2019, 10 (1), 4829-4835. 

　　2. Liu D.; Yu, W. B; Deng L. L.; Yuan, W. W.; Sun H. J.; Ma, L. Y.; Yuan, P.; Du P. X.; He H. P. Possible mechanism of structural incorporation of Al into diatomite during the deposition process I. Via a condensation reaction of hydroxyl groups. Journal of Colloid Interface Science. 2016, 461, 64-68. 

　　3. Liu, D.; Yuan, P. ; Liu, H. M.; Cai, J. G.; Qin, Z. H.; Tan, D. Y.; Zhou, Q.; He, H. P.; Zhu, J. X.; Quantitative characterization of the solid acidity of montmorillonite using combined FTIR and TPD based on the NH3 adsorption. Applied Clay Science. 2013. 80-81, 407-412.  

　　4. Liu, D.; Yuan, P. ; Liu, H. M.; Cai, J. G.; Qin, Z. H.; Tan, D. Y.; Zhou, Q.; He, H. P.; Zhu, J. X., Influence of heating on the solid acidity of montmorillonite: A combined study by DRIFT and Hammett indicators. Applied Clay Science. 2011, 52 (4), 358-363. 

　　5. Liu, D.; Yuan, P.; Liu, H. M; Tian L.; Tan, D. Y.; Yuan, W.W.; He, H P; High-pressure adsorption of methane on montmorillonite, kaolinite and illite. Applied Clay Science, 2013, 85, 25-30. 

　　  

　　刘 锦，男，1984年1月生，北京高压科学研究中心研究员，博士 

　　请奖项目：地球深部含水含碳物质的高温高压实验研究  

　　与请奖项目有关的主要学术成就与创新点：①通过研究铁碳合金和碳酸盐矿物的高温高压行为，对重新认识地球内部潜在含碳载体有重要指示意义；②在地球核幔边界温压条件下，首次揭示水与铁核发生新型高压化学反应，并形成含氢过氧化铁富集区域，对核幔边界超低波速带提供了全新的成因解释；③通过对含水含碳俯冲物质演化的研究，揭示了在深下地幔环境中氧元素的价态在-1和-2之间可变，有助于形成富氧物质并导致下地幔化学不均一性，为深入理解板片-地幔相互作用过程及效应提供了强有力的矿物学约束。 

　　五篇代表性论著：  

　　1.J. Liu, Q. Hu, W. Bi, L. Yang, Y. Xiao, P. Chow, Y. Meng, V.B. Prakapenka, H.K. Mao, W.L. Mao (2019), Altered chemistry of oxygen and iron under deep Earth conditions. Nature Commun. 10, 153. 

　　2.J. Liu, Q. Hu, D.Y. Kim, Z. Wu, W. Wang, Y. Xiao, P. Chou, Y. Meng, V.B. Prakapenka, H.K. Mao, W.L. Mao (2017), Hydrogen-bearing iron peroxide and the origin of ultralow-velocity zones. Nature 551, 494-497. 

　　3. J. Liu, N. Dauphas, M. Roskosz, M.Y. Hu, H. Yang, W. Bi, J. Zhao, E.E. Alp, J. Hu, J.F. Lin (2017), Iron isotopic fractionation between silicate mantle and metallic core at high pressure. Nature Commun. 8, 14377. 

　　4. J. Liu, J.F. Lin, V.B. Prakapenka, C. Prescher, T. Yoshino (2016), Phase relations of Fe3C and Fe7C3 up to 185 GPa and 5200 K: Implication for the stability of iron carbide in the Earth's core. Geophys. Res. Lett. 43, 12415-12422. 

　　5. J. Liu, J.F. Lin (2014), Abnormal acoustic wave velocities in basaltic and (Fe,Al)-bearing silicate glasses at high pressures. Geophys. Res. Lett. 41, 8832-8839. 

　　  

　　岩 石 学 组 

　　戴立群，男，1986年2月生，中国科学技术大学特任教授，博士 

　　请奖项目：造山带镁铁质岩浆作用  

　　与请奖项目有关的主要学术成就与创新点：① 识别和区分出从洋壳俯冲到大陆碰撞过程中两类壳幔相互作用的鉴定性指标，揭示了碰撞造山带形成过程中不同类型壳幔相互作用的化学地球动力学机制；② 将稀有气体同位素与全岩地球化学特征相结合，提出稀有气体再循环可以在大陆俯冲带通过板片-地幔相互作用来实现；③ 识别出俯冲地壳来源的不同性质的熔流体，及其熔体-橄榄岩反应所形成的不均一的地幔岩石学性质。 

　　五篇代表性论著： 

　　1. Dai, L.-Q., Zhao, Z.-F.*, Zheng, Y.-F., Li, Q., Yang, Y., Dai, M., 2011. Zircon Hf-O isotope evidence for crust-mantle interaction during continental deep subduction. Earth and Planetary Science Letters 308, 224-244. 

　　2. Dai, L.-Q., Zhao, Z.-F.*, Zheng, Y.-F., Zhang, J., 2012. The nature of orogenic lithospheric mantle: geochemical constraints from postcollisional mafic-ultramafic rocks in the Dabie orogen. Chemical Geology 334, 99-121. 

　　3. Dai, L.-Q.*, Zhao, Z.-F., Zheng, Y.-F., An, Y.J., Zheng, F., 2017. Geochemical distinction between carbonate and silicate metasomatism in generating the mantle sources of alkali basalts. Journal of Petrology 58, 863-884. 

　　4. Dai, L.-Q.*, Zheng, F., Zhao, Z.-F., Zheng, Y.-F., 2017. Recycling of Paleotethyan oceanic crust: Geochemical record from postcollisional mafic igneous rocks in the Tongbai-Hong’an orogens, Geological Society of America Bulletin 129(1- 2), 179-192. 

　　5. Dai, L.-Q.*, Zheng, F., Zhao, Z.-F., Zheng, Y.-F., 2018. Geochemical insights into the lithology of mantle sources for Cenozoic alkali basalts in West Qinling, China. Lithos 302-303, 86-98 

　　  

　　郭 顺,男，1982年9月生,中国科学院地质与地球物理研究所副研究员, 博士 

　　请奖项目：俯冲带变质流体演化和元素迁移  

　　与请奖项目有关的主要学术成就与创新点：①提出检验榴辉岩中硬柱石早期存在的新方法和岩石学指示标志。阐明大陆俯冲带硬柱石榴辉岩变质脱水的条件、过程和物理-化学效应。②率先开展俯冲带变质岩中绿帘石综合研究，揭示俯冲带流体的源区、成分、氧逸度、运移方式和演化历史。研发绿帘石原位Sr同位素分析方法并应用于变质流体示踪。③首次发现富电气石的超高压榴辉岩-脉体系统，揭示不纯大理岩是俯冲板片中高δ11B流体的储库。④创建复杂开放地质体系元素迁移的计算-图解方法，揭示俯冲带水/岩反应机理和元素迁移规律，为认识俯冲带元素活动性和板片-幔-弧物质循环提供重要科学依据。 

　　五篇代表性论著：  

　　1. Guo, S., Zhao, K.D., John, T., Tang, P., Chen, Y., Su, B., 2019. Metasomatic flow of metacarbonate-derived fluids carrying isotopically heavy boron in continental subduction zones: Insights from tourmaline-bearing ultra-high pressure eclogites and veins. Geochimica et Cosmochimica Acta, 253, 159-200. 

　　2. Guo, S., Tang, P., Su, B., Chen, Y., Ye, K., Zhang, L.M., Gao, Y.J., Liu, J.B., Yang, Y.H., 2017. Unusual replacement of Fe-Ti oxides by rutile during retrogression in amphibolite-hosted veins: A mineralogical record of fluid-induced oxidation processes in exhumed UHP slabs. American Mineralogist, 102, 2268-2283. 

　　3. Guo, S., Ye, K., Yang, Y.H., Chen, Y., Zhang, L.M., Liu, J.B., Mao, Q., Ma, Y.G., 2014. In situ Sr isotopic analyses of epidote: tracing the sources of multi-stage fluids in ultrahigh-pressure eclogite. Contributions to Mineralogy and Petrology. DOI: 10.1007/s00410-014-0975-9. 

　　4. Guo, S., Ye, K., Wu, T.F., Chen, Y., Yang, Y.H., Zhang, L.M., Liu, J.B., Mao, Q., Ma, Y.G., 2013. A potential method to confirm the previous existence of lawsonite in eclogite: the mass imbalance of Sr and LREEs in multistage epidote. Journal of Metamorphic Geology, 31, 415-435. 

　　5. Guo, S., Ye, K., Chen, Y., Liu, J.B., 2009. A normalization solution to mass transfer illustration of multiple progressively altered samples using the Isocon diagram. Economic Geology, 104, 881-886.  

　　  

　　李金祥，男，1981年6月生，中国科学院青藏高原研究所副研究员，博士 

　　请奖项目：青藏高原及邻区中-新生代特提斯构造演化-岩浆及成矿作用 

　　与请奖项目有关的主要学术成就与创新点：①揭示班公湖带多龙超大型斑岩-高硫型浅成低温热液Cu-Au系统的结构及其过渡机制，并提出该带俯冲-碰撞斑岩-矽卡岩Cu±Mo±Au成矿作用的地球动力学模式；②揭示了青藏高原后碰撞背景成矿斑岩继承了早期俯冲岛弧阶段岩浆形成斑岩型铜矿床的能力；③系统建立了青藏高原邻区缅甸中-新生代构造演化-岩浆-成矿作用的模式。 

　　五篇代表性论著： 

　　1. Li, J.X., Qin, K.Z., Li, G.M., Evans, N.J., Huang, F., Zhao, J.X., 2018. Iron isotope fractionation during magmatic-hydrothermal evolution: A case study from the Duolong porphyry Cu-Au deposit, Tibet. Geochimica Et Cosmochimica Acta 238, 1-15. 

　　2. Li, J.-X., Qin, K.-Z., Li, G.-M., Evans, N.J., Zhao, J.-X., Yue, Y.-H., Xie, J., 2018. Volatile variations in magmas related to porphyry Cu-Au deposits: Insights from amphibole geochemistry, Duolong district, central Tibet. Ore Geology Reviews 95, 649-662. 

　　3. Li, J. X., Qin, K.-Z., Li, G.-M., Evans, N.J., Zhao, J.-X., Cao, M.-J., Huang, F., 2016. The Nadun Cu–Au mineralization, central Tibet: Root of a high sulfidation epithermal deposit. Ore Geology Reviews 78, 371-387. 

　　4. Li, J.X., Qin, K.Z., Li, G.M., Xiao, B., Zhao, J.X., Cao, M.J., Chen, L., 2013. Petrogenesis of ore-bearing porphyries from the Duolong porphyry Cu–Au deposit, central Tibet: Evidence from U–Pb geochronology, petrochemistry and Sr-Nd-Hf-O isotope characteristics. Lithos, 160–161: 216-227. 

　　5. Li, J.X., Qin, K.Z., Li, G.M., Xiao, B., Chen, L., Zhao, J.X., 2011. Post-collisional ore-bearing adakitic porphyries from Gangdese porphyry copper belt, southern Tibet: Melting of thickened juvenile arc lower crust. Lithos, 126(3-4): 265-277. 

　　  

　　刘 佳，男，1985年11月生，浙江大学地球科学学院研究员，博士 

　　请奖项目：挥发分在板内玄武岩形成中的作用 

　　与请奖项目有关的主要学术成就与创新点：①揭示了太平洋板块俯冲对华北地幔的持续水化作用，为理解中生代华北克拉通的破坏机制及新生代玄武岩的形成过程提供了新制约；②揭示了峨眉山大火成岩省源区显著富水的特征，为认识水在大火成岩省形成过程中的作用提供了关键证据；③揭示了古老太平洋板块上小火山的形成与碳酸岩化熔体密切相关，为理解大洋岩石圈-软流圈界面的成因提供了新信息。 

　　五篇代表性论著： 

　　1. Liu, J.*, Hirano, N., Machida, S., Xia, Q.K., Tao, C.H., Liao, S.L., Liang, J., Li, W., Yang, W.F., Zhang, G.Y., Ding, T., 2020. Melting of recycled ancient crust responsible for the Gutenberg discontinuity. Nature Communications 11, 172. Doi:10.1038/s41467-019-13958-w. 

　　2.Liu, J.*, Xia, Q.K.*, Kuritani, T., Hanski, E., Yu, H.R., 2017. Mantle hydration and the role of water in the generation of large igneous provinces. Nature Communications 8, 1824. Doi:10.1038/s41467-017-01940-3. 

　　3. Liu, J., Xia, Q.K.*, Deloule, E., Ingrin, J., Chen, H., Feng, M., 2015. Water content and oxygen isotopic composition of alkali basalts from the Taihang Mountains, China: recycled oceanic components in the mantle source. Journal of Petrology 56, 681-702. 

　　4. Liu, J.*, Xia, Q.K.*, Deloule, E., Chen, H., Feng, M., 2015. Recycled oceanic crust and marine sediment in the source of alkali basalts in Shandong, eastern China: Evidence from magma water content and oxygen isotopes. Journal of Geophysical Research: Solid Earth 120, 8281-8303. 

　　5. Liu, J.*, Wang, Z.Z., Yu, H.R., Xia, Q.K., Deloule, E., Feng, M., 2017. Dynamic contribution of recycled components from the subducted Pacific slab: Oxygen isotopic composition of the basalts from 106 Ma to 60 Ma in North China Craton. Journal of Geophysical Research: Solid Earth 122, 988-1006. 

　　  

　　熊 庆，男，1986年7月生，中国地质大学（武汉）教授，博士 

　　请奖项目：地质体橄榄岩成因与地幔演化 

　　与请奖项目有关的主要学术成就与创新点：① 发现青藏高原南部雅江带泽当蛇绿岩具有双层地幔结构，提出新特提斯洋经历两阶段“弧前岩石圈增生”的新模型，揭示了大洋扩张中心地幔内复杂的岩浆反应迁移过程，为解释大洋壳-幔Os同位素解耦现象提供了创新思路；② 揭示了青藏高原柴北缘造山带橄榄岩的克拉通地幔起源及其在俯冲带地幔楔内经历的复杂交代和岩浆过程，发现大陆地幔楔的改造与超大陆“聚-裂”演化具有内在关联，为大陆生存和消亡机制提供了新认识。 

　　五篇代表性论著：  

　　1. Xiong Qing, Xu Yong, Gonzalez-Jimenez J.M., Liu Jingao, Alard O., Zheng Jian-Ping, Griffin W.L., O'Reilly S.Y., 2020. Sulfide in dunite channels reflects long-distance reactive migration of mid-ocean-ridge melts from mantle source to crust: A Re-Os isotopic perspective. Earth and Planetary Science Letters, 531, 115969, doi: 10.1016/j.epsl.2019.115969. 

　　2. Xiong Qing, Griffin W.L., Zheng Jian-Ping, O'Reilly S.Y., Pearson N.J., Xu Bo, Belousova E.A., 2016. Southward trench migration at ～130-120 Ma caused accretion of the Neo-Tethyan forearc lithosphere in Tibetan ophiolites. Earth and Planetary Science Letters, 438, 57-65. 

　　3. Xiong Qing, Zheng Jian-Ping, Griffin W.L., O'Reilly S.Y., Pearson N.J., 2014. Pyroxenite dykes in orogenic peridotite from North Qaidam (NE Tibet, China) track metasomatism and segregation in the mantle wedge. Journal of Petrology, 55, 2347-2376. 

　　4. Xiong Qing, Henry H., Griffin W.L., Zheng Jian-Ping, Satsukawa T., Pearson N.J., O'Reilly S.Y., 2017. High- and low-Cr chromitite and dunite in a Tibetan ophiolite: evolution from mature subduction system to incipient forearc in the Neo-Tethyan Ocean. Contributions to Mineralogy and Petrology, 172: 45. 

　　5. Xiong Qing, Griffin W.L., Zheng Jian-Ping, O'Reilly S.Y., Pearson N.J., 2015. Episodic refertilization and metasomatism of Archean mantle: evidence from an orogenic peridotite in North Qaidam. Contributions to Mineralogy and Petrology, 169: 31. 

　　  

　　地球化学一组 

　　黄康俊，男，1985年5月生，西北大学地质学系教授，博士 

　　请奖项目：表生地质过程镁同位素地球化学 

　　与请奖项目有关的主要学术成就与创新点：①对大陆风化作用，风尘沉积，白云岩沉积，洋壳低温蚀变作用等表生地质过程镁同位素行为进行了系统研究，有效加深了对全球镁地球化学循环过程的认识，为应用镁同位素示踪地质过程奠定了理论基础；②率先利用碎屑沉积岩镁同位素体系示踪古化学风化作用，对新元古代全球冰期结束过程化学风化作用进行制约，提出“雪球地球”事件结束机制新模式；③建立了中国黄土次生碳酸盐镁同位素与东亚季风降水之间的定量关系，为古气候参数定量重建及气候变化预测提供了新思路。 

　　五篇代表性论著： 

　　1. Huang, K.-J., Teng, F.-Z., Plank, T., Staudigel, H., Hu, Y., Bao, Z.-Y., 2018. Magnesium isotopic composition of altered oceanic crust and the global Mg cycle. Geochimica et Cosmochimica Acta 238, 357-373. 

　　2. Huang, K.-J., Teng, F.-Z., Shen, B., Xiao, S., Lang, X.-G., Ma, H.-R., Fu, Y. and Peng, Y.-B., 2016. Episode of intense chemical weathering during the termination of the 635 Ma Marinoan glaciation, Proceedings of the National Academy of Sciences 113, 14904-14909. 

　　3. Huang, K.-J., Shen B., Lang X.-G., Tang W.-B., Peng Y., Ke S., Ma H.-R., Li F.-B., 2015. Magnesium isotopic compositions of the Mesoproterozoic dolostones: Implications for Mg isotopic systematics of marine carbonates. Geochimica et Cosmochimica Acta 164, 333-351. 

　　4. Huang, K.-J., Teng, F.-Z., Elsenouy, A., Li, W.-Y, Bao, Z.-Y., 2013. Magnesium isotopic variations in loess: Origins and implications. Earth and Planetary Science Letters 374, 60-70. 

　　5. Huang, K.-J., Teng, F.-Z., Wei, G.-J., Ma, J.-L., Bao, Z.-Y., 2012. Adsorption- and desorption-controlled magnesium isotope fractionation during extreme weathering of basalt in Hainan Island, China. Earth and Planetary Science Letters 359-360, 73-83. 

　　  

　　刘 羿，男，1981年12月生，天津大学地球系统科学学院教授，博士 

　　请奖项目：表生地球化学 

　　主要学术成就与创新点：①通过珊瑚高精度硼同位素研究，揭示了7千以来南海珊瑚礁区海水pH值的自然波动规律，阐述了近代南海海洋酸化过程的控制机理；②通过分析珊瑚与有孔虫的稀土、钕同位素组成，揭示了过去28万年西太赤道辐合带迁移规律，发现极端低压是在地球高倾角时形成，而不是传统观点认为的岁差控制的太阳辐射最大值时，表明倾角对全球水汽循环的影响比过去假设的要大得多；③系统测定了南海珊瑚的钡同位素组成，发现不同采样地点的珊瑚和海水间钡同位素分馏基本恒定，不受温度等外部环境和珊瑚生物矿化的影响，开启了钡同位素指示古海洋生产力变化的新应用。 

　　五篇代表性论著： 

　　1. Yi Liu，Li Lo，Zhengguo Shi，Kuo-Yen Wei，Chien-Ju Chou，Yi-Chi Chen，Chih-Kai Chuang，Chung-Che Wu，Horng-Sheng Mii，Zicheng Peng，Hiroshi, Amakawa，George S. Burr，Shih-Yu Lee，Kristine L. DeLong，Henry Elderfield，Chuan-Chou Shen，Obliquity pacing of the western Pacific Intertropical Convergence Zone over the past 282,000 years，Nature Communications，2015，6，DOI: 10.1038/ncomms10018 

　　2. Yi Liu , Xiaohua Li , Zhen Zeng , Hui-Min Yu , Fang Huang, Thomas Felis, Chuan-Chou Shen. Annually-resolved coral skeletal d138/134Ba records: A new proxy for oceanic Ba cycling, Geochimica et Cosmochimica Acta, 2019,247 27-39 

　　3. Yi Liu，Weiguo Liu，Zicheng Peng，Yingkai Xiao，Gangjian Wei，Weidong Sun，Jianfeng He，Guijian Liu，Chen-Lin Chou，Instability of seawater pH in the South China Sea during the mid-late Holocene: Evidence from boron isotopic composition of corals，Geochimica et Cosmochimica Acta，2009，73(5):1264-1272 

　　4. Yi Liu，Zicheng Peng，Chuanchou Shen，Renjun Zhou，Shaohua Song，Zhengguo Shi，Tegu Chen，Gangjian Wei，Kristine L. DeLong，Recent 121-year variability of western boundary upwelling in the northern South China Sea, Geophysical Research Letter，2013，40, doi:10.1002/grl.50381 

　　5. Yi Liu ，Zicheng Peng，Tegu Chen，Weidong Sun，Ruoyu Sun，Jianfeng He，Guijian Liu，Chen-Lin Chou，Robert E. Zartman，The decline of winter monsoon velocity in the South China Sea through the 20th century: Evidence from the Sr/Ca records in corals，Global and Planetary Change，2008，63（1）：79-85 

　　  

　　刘媛媛，女，1980年5月生，南京大学地球科学与工程学院特聘研究员，博士 

　　请奖项目：土壤和地下水污染的水文-多元素生物地球化学耦合过程研究  

　　与请奖项目有关的主要学术成就与创新点：①揭示河床内微生物群落驱动氮循环的时空演变机制，构建基于过程的水文-多元素生物地球化学反应耦合模型，预测河床潜流带阻滞铬的生态功能；②首次研制出具有表面电异性的微流体，为电异性多孔介质内的微生物迁移研究提供了新的实时观测技术，并提出了控制土壤和沉积物等电异性介质拦截微生物的新机制；③首次观察并解释了锝还原反应速率常数的反常尺度效应，采用微流体模拟孔隙尺度非均质传质，进行多尺度建模，成功解决了地下环境非均质性造成的锝和铁反应速率常数的尺度提升难题，推动地下水生物地球化学过程反应参数的尺度提升研究。 

　　五篇代表性论著： 

　　1. Fen Xu#; Yuanyuan Liu#; Chongxuan Liu*; A generalized-rate model for describing and scaling redox kinetics in sediments containing variable redox-reactive materials, Environmental Science & Technology, 2018, 52: 5268~5276 

　　2. Yuanyuan Liu#; Fen Xu#; Chongxuan Liu*; Coupled hydro-biogeochemical processes controlling Cr reductive immobilization in Columbia River hyporheic zone, Environmental Science & Technology, 2017, 51(3): 1508~1517  

　　3. Yuanyuan Liu; Chongxuan Liu*; William C. Nelson; Shi Liang; Fen Xu; Yunde Liu; Ailan Yan; Lirong Zhong; Christopher Thompson; James K. Fredrickson; John M. Zachara; Effect of water chemistry and hydrodynamics on nitrogen transformation activity and microbial community functional potential in hyporheic zone sediment columns, Environmental Science & Technology, 2017, 51(9): 4877~4886 

　　4. Fen Xu; Yuanyuan Liu*; John Zachara; Mark Bowden; David Kennedy; Andrew E. Plymale; Chongxuan Liu*; Redox transformation and reductive immobilization of Cr(VI) in the Columbia River hyporheic zone sediments, Journal of Hydrology, 2017, 555: 278~287  

　　5. Yuanyuan Liu; Chongxuan Liu*; Changyong Zhang; Xiaofan Yang; John M. Zachara; Pore and continuum scale study of the effect of subgrid transport heterogeneity on redox reaction rates, Geochimica et Cosmochimica Acta, 2015, 163: 140~155 

　　  

　　孙 静，女，1987年1月生，中国科学院地球化学研究所研究员，博士 

　　请奖项目：铁循环与重金属相互作用的地球化学机制  

　　与请奖项目有关的主要学术成就与创新点：① 解析铁矿物相重组对砷溶解度的影响，提出通过原位生成磁铁矿进行地下水砷污染修复的新方法，有望改善分散型砷暴露人群的水安全问题；② 率先开展新兴环境毒物钨的环境水文地球化学研究，揭示聚钨酸根在铁矿物表面弱吸附是钨溶解度异常高的重要原因，为场地地下水钨污染研究提供理论基础；③ 完善地下水系统中铁循环过程及其影响下重金属释放-固定过程的模拟计算方法，实现水质控制过程的精准量化，为污染成因识别和治理技术研发提供依据。 

　　五篇代表性论著： 

　　1.David Schafer#, Jing Sun*, James Jamieson, Adam Siade, Olivier Atteia, and Henning Prommer*. (2020). Model-based analysis of reactive transport processes governing fluoride and phosphate release and attenuation during managed aquifer recharge. Environmental Science & Technology, 54(5): 2800-2811. 

　　2.Henning Prommer#,*, Jing Sun*, Lauren Helm, Bhasker Rathi, Adam Siade, and Ryan Morris. (2018). Deoxygenation prevents arsenic mobilization during deepwell injection into sulfide-bearing aquifers. Environmental Science & Technology, 52(23): 13801-13810. 

　　3.Jing Sun#, Henning Prommer*, Adam Siade, Steven Chillrud, Brian Mailloux, and Benjamín Bostick. (2018). Model-based analysis of arsenic immobilization via iron mineral transformation under advective flows. Environmental Science & Technology, 52(16): 9243-9253. 

　　4.Benjamín Bostick#,*, Jing Sun*, Joshua Landis, and Jay Clausen. (2018). Tungsten speciation and solubility in munitions-impacted soils. Environmental Science & Technology, 52(3): 1045-1053. 

　　5.Jing Sun#, Steven Chillrud, Brian Mailloux, and Benjamín Bostick*. (2016). In situ magnetite formation and long-term arsenic immobilization under advective flow conditions. Environmental Science & Technology, 50(18): 10162-10171. 

　　  

　　地球化学二组 

　　陈伊翔，男，1983年3月生，中国科学技术大学教授，博士 

　　请奖项目：大陆俯冲带变质地球化学 

　　与请奖项目有关的主要学术成就与创新点：①在苏鲁造山带首次发现~3.7 Ga岩浆锆石，揭示了变质和深熔过程对锆石O-Hf同位素体系的影响；②系统查明了超高压变质岩部分熔融的证据、时限、熔融反应和熔体组成特征，限定了熔体组成的控制因素，揭示了矿物尺度巨大Nb/Ta分异及其机制；③厘清了西阿尔卑斯造山带白片岩的原岩属性，利用O-Mg-Fe同位素率先发现蛇纹岩来源的还原性流体对深俯冲陆壳的反向交代作用，揭示了富镁碳酸盐在弧前深度存在显著溶解，极大深化了对俯冲带流体性质的认识。  

　　五篇代表性论著： 

　　1. Chen, Y.-X.*, Demeny, A., Schertl, H.-P., Zheng, Y.-F., Huang, F., Zhou, K., Jin, Q.-Z., Xia, X.-P., 2020. Tracing subduction zone fluids with distinct Mg isotope compositions: Insights from high-pressure metasomatic rocks (leucophyllites) from the Eastern Alps. Geochimica et Cosmochimica Acta 271, 154-178. 

　　2. Chen, Y.-X.*, Lu, W.N., He, Y.S.*, Schertl, H.P., Zheng, Y.-F., Xiong, J.-W., Zhou, K., 2019. Tracking Fe mobility and Fe speciation in subduction zone fluids at the slab-mantle interface in a subduction channel: A tale of whiteschist from the Western Alps. Geochimica et Cosmochimica Acta 267, 1-16. 

　　3. Chen, Y.X.*, Schertl, H.-P., Zheng, Y.-F., Huang, F., Zhou, K., Gong, Y.-Z., 2016. Mg-O isotopes trace the origin of Mg-rich fluids in the deeply subducted continental crust of Western Alps. Earth and Planetary Science Letters 456, 157-167. 

　　4. Chen, Y.-X.*, Zheng, Y.-F., 2015. Extreme Nb/Ta fractionation in metamorphic titanite from ultrahigh-pressure metagranite. Geochimica et Cosmochimica Acta 150, 53-73. 

　　5. Chen, Y.-X., Zheng, Y.-F.*, Chen, R.-X., Zhang, S.-B., Li, Q., Dai, M., Chen, L., 2011. Metamorphic growth and recrystallization of zircons in extremely 18O-depleted rocks during eclogite-facies metamorphism: Evidence from U-Pb ages, trace elements, and O-Hf isotopes. Geochimica et Cosmochimica Acta 75, 4877-4898. 

　　  

　　凌宗成，男，1981年4月生，山东大学（威海）空间科学与物理学院/空间科学研究院教授，博士 

　　请奖项目：行星物质光谱遥感与实验研究 

　　与请奖项目有关的主要学术成就与创新点：①利用嫦娥三号“玉兔号”月球车探测数据发现了新型月球玄武岩，揭示了月球雨海年轻火山活动的特殊岩浆演化机制，为月球轨道遥感研究提供了新的月面真值；②建立了基于嫦娥探测光谱数据的月表物质成分反演和岩石类型分布填图方法，为认识月球岩石成因和岩浆演化提供了重要线索；③推动和拓展拉曼光谱学在阿波罗月球样品和陨石实验研究中的应用，论证了拉曼光谱应用于月球就位探测及资源利用的可行性；④开展含水硫酸铁等火星模拟盐类的实验室合成、光谱学表征及热动力学研究，为火星遥感和就位探测相关数据解译提供了基础光谱库和实验约束。 

　　五篇代表性论著： 

　　1) Ling Z*, Jolliff B L, Wang A, Li C, Liu J, Zhang J, Li B, Sun L, Chen J, Xiao L, Liu J, Ren X, Peng W, Wang H, Cui X, He Z, and Wang J. (2015) Correlated compositional and mineralogical investigations at the Chang'e-3 landing site. Nature Communications, 6: 8880. 

　　2) Ling Z*, Wang A. (2015) Spatial distributions of secondary minerals in the Martian meteorite MIL 03346,168 determined by Raman spectroscopic imaging. Journal of Geophysical Research Planets, 120(6):1141-1159. 

　　3) Ling Z*, Cao F, Ni Y, Wu Z, Zhang J, Li B. (2016) Correlated analysis of chemical variations with spectroscopic features of the K–Na jarosite solid solutions relevant to Mars. Icarus, 271, 19-29. 

　　4) Ling Z*, Wang A, Jolliff B L. (2011) Mineralogy and geochemistry of four lunar soils by laser-Raman study. Icarus, 211(1):101-113. 

　　5) Ling Z*, Wang A. (2010) A systematic spectroscopic study of eight hydrous ferric sulfates relevant to Mars. Icarus, 209(2): 422–433. 

　　6) Sun L, Ling Z*. (2015) Partial Least Squares Modeling of Lunar Surface FeO Content with Clementine Ultraviolet-Visible Images. Chapter 1. In S. Jin et al. (eds.), Planetary Exploration and Science: Recent Results and Advances, Springer Geophysics, 1-19, DOI 10.1007/978-3-662-45052-9_1. 

　　  

　　张 鑫，男，1981年5月生，中国科学院海洋研究所研究员，博士 

　　请奖项目：深海原位拉曼光谱技术研发及应用  

　　请奖项目有关的主要学术成就与创新点：①突破了普通光学镜头不耐高温和防颗粒附着性能差等技术难点，研制了系列化的深海原位激光拉曼光谱探针；②通过在实验室构建深海高温高压环境模拟装置，建立了针对深海极端环境的激光拉曼光谱原位定量分析技术体系；③综合应用系列化原位拉曼光谱探针和拉曼定量分析方法，在我国南海发现裸露在海底的可燃冰;在深海热液区发现自然状态下存在超临界二氧化碳和气态水;发现全球深海沉积物中甲烷被低估约20倍。 

　　五篇代表性论著： 

　　1.Xin Zhang*, Lian-fu Li, Zeng-feng Du, Xi-luo Hao, Lei Cao Zhen-dong Luan, Bing Wang, Shi-chuan Xi, Chao Lian, Jun Yan, Wei-dong Sun*. Discovery of supercritical carbon dioxide in a hydrothermal system. Science Bulletin. 2020, DOI: 10.1016/j.scib.2020.03.023. 

　　2. Xin Zhang, K.C. Hester, W. Ussler, P. Walz, E.T. Peltzer, and P.G. Brewer. In situ Raman-based measurements of high dissolved methane concentrations in hydrate-rich ocean sediments. Geophysical Research Letters, 2011, 38:L08605. 

　　3. Xin Zhang？, Zengfeng Du, Ronger Zheng, Zhendong Luan , Fujun Qi, Kai Cheng , Bing Wang, Wangquan Ye, Xiaorui Liu , Chao Lian , Changan Chen, Jinjia Guo , Ying Li , Jun Yan. Development of a new deep-sea hybrid Raman insertion probe and its application to the geochemistry of hydrothermal vent and cold seep fluids. Deep Sea Research Part I Oceanographic Research Papers, 2017, 123:1-12. 

　　4. Lianfu Li, Xin Zhang*, Zhendong Luan, Zengfeng Du, Shichuan Xi, Bing Wang, Chao Lian, Lei Cao, Jun Yan. Hydrothermal vapor‐phase fluids on the seafloor: evidence from in situ observations. Geophysical Research Letters, 2020. 47, e2019GL085778. https://doi.org/10.1029/2019GL085778 

　　5. Lianfu Li, Xin Zhang*, Zhendong Luan, Zengfeng Du, Shichuan Xi, Bing Wang, Lei Cao, Chao Lian, Jun Yan (2018). In situ quantitative Raman detection of dissolved carbon dioxide and sulfate in deep-sea high-temperature hydrothermal vent fluids. Geochemistry, Geophysics, Geosystems, 2018, 19(6): 1809-1823.  

　　  

　　郑 旺，男，1981年9月生，天津大学地球系统科学学院教授，博士 

　　请奖项目：汞稳定同位素分馏机理及其应用 

　　与请奖项目有关的主要学术成就与创新点：① 率先确定了关键环境地球化学过程中的汞同位素分馏系数和机理，建立了汞同位素分馏的核心理论框架，为汞同位素在解析污染来源、示踪环境过程和重建环境与生命演化等领域的广泛应用奠定了基础；② 提出了古海洋硫化现象的汞同位素新指标，揭示了汞同位素在重建古海洋氧化还原环境方面的应用潜力，对进一步利用汞及其它金属同位素研究地球环境与生命协同演化具有重要指示意义；③基于汞同位素揭示了森林、极地等地球表层生态系统中汞的来源、循环机制和环境影响；④ 发现了汞在厌氧环境中的氧化还原和甲基化新机制，促进了对汞的生物可利用性和环境健康效应的研究。 

　　五篇代表性论著：  

　　1. Zheng, W.*; Gilleaudeau, G. J.; Kah, L. C.; Anbar, A. D., Mercury isotope signatures record photic zone euxinia in the Mesoproterozoic ocean. Proc. Natl. Acad. Sci. USA 2018, 115, 10594-10599.  

　　2. Zheng, W.*; Hintelmann, H., Mercury isotope fractionation during photoreduction in natural water is controlled by its Hg/DOC ratio. Geochim. Cosmochim. Acta 2009, 73, 6704-6715.  

　　3. Zheng, W.*; Demers, J.; Lu, X.; Bergquist, B. A.; Anbar, A. D.; Blum, J. D.; Gu, B.*, Mercury stable isotope fractionation during abiotic dark oxidation in the presence of thiols and natural organic matter. Environ. Sci. Technol. 2019, 53(4), 1853-1862.  

　　4. Zheng, W.*; Obrist, D.; Weis, D.; Bergquist, B. A., Mercury isotope compositions across North American forests. Global Biogeochem. Cycles, 2016, 30, 1475–1492.  

　　5. Zheng, W.*; Liang, L; Gu, B.*, Mercury reduction and oxidation by reduced natural organic matter in anoxic environments. Environ. Sci. Technol. 2012, 46, 292-299.  

　　  

　　地球化学三组 

　　李 诺，女，1984年3月生，中国科学院新疆生态与地理研究所新疆矿产资源研究中心研究员，博士 

　　请奖项目：秦岭钼矿成矿规律 

　　与请奖项目有关的主要学术成就与创新点：①首次发现了多子晶富CO2包裹体，颠覆了富CO2流体盐度低、不能形成贱金属矿床的传统观点；②发现秦岭-大别造山带燕山期斑岩型钼矿不同于已知陆缘弧型和弧后裂谷型，而是新类型的斑岩钼矿—碰撞型；③发现18.5亿年钼成矿事件，揭示东秦岭钼超常富集的三大原因是：发育前寒武纪富钼基底、存在多期多类型钼矿化、燕山期碰撞-后碰撞体制的岩浆-流体作用。 

　　五篇代表性论著： 

　　1. Li N, Chen, Y.J., Santosh, M., Pirajno, F., 2018. Late Mesozoic granitoids in the Qinling Orogen, Central China, and tectonic significance. Earth-Science Reviews, 182: 141-173 

　　2. Li, N., Ulrich, T., Chen, Y.J., Thomsen, T.B., Pease, V., Pirajno, F., 2012. Fluid evolution of the Yuchiling porphyry Mo deposit, East Qinling, China. Ore Geology Reviews, 48: 442-459 

　　3. Li, N., Chen, Y.J., Ulrich, T., Lai, Y., 2012. Fluid inclusion study of the Wunugetu Cu-Mo deposit, Inner Mongolia, China. Mineralium Deposita, 47: 467-462 

　　4. Li, N., Chen, Y.J., Santosh, M., Yao, J.M., Sun, Y.L., Li, J., 2011. The 1.85 Ga Mo mineralization in the Xiong￠er Terrane, China: Implications for metallogeny associated with assembly of the Columbia supercontinent. Precambrian Research, 186: 220-232 

　　5. Li, N., Chen, Y.J., Santosh, M., Pirajno, F., 2015. Compositional polarity of Triassic granitoids in the Qinling Orogen, China: Implication for termination of the northernmost paleo-Tethys. Gondwana Research, 27: 244-257 

　　  

　　刘 琰 ，男，1982年8月生，中国地质科学院地质研究所研究员，博士 

　　请奖项目：碳酸岩型稀土矿床中稀土元素的超常富集过程  

　　与请奖项目有关的主要学术成就与创新点：①发现成矿碳酸岩来自岩石圈地幔，而非地幔柱，富CO₂-REE俯冲板片流体交代岩石圈地幔，使REE在地幔源区初始富集；②揭示REE在岩浆-热液系统中再次富集，提出温度降低导致REE络合物分解是REE在热液阶段晚期大规模沉淀的重要机制；③建立了碳酸岩型REE矿床关键的成矿模式，该模型强调，碳酸岩型稀土矿床的形成必须经历岩浆阶段的初始富集和岩浆-热液过程的再次富集；揭示了碳酸岩型稀土矿床的成矿过程和成矿机理。 

　　五篇代表性论著： 

　　1. Liu, Y*., Hou, Z.Q, Zhang, R.Q., Wang, P., Gao, J.F., Raschke, M.B., 2019b. Zircon Alteration as a Proxy for Rare Earth Element Mineralization Processes in Carbonatite-Nordmarkite Complexes of the Mianning-Dechang Rare Earth Element Belt, China. Economic Geology, 114, 719-744.  

　　2. Liu, Y., Chakhmouradian, A.R., Hou, Z.Q., Song, W.L., Kynicky, J., 2019a. Development of REE mineralization in the giant Maoniuping deposit (Sichuan, China): insights from mineralogy, fluid inclusions, and trace-element geochemistry. Mineralium Deposita, 54, 701-718.  

　　3. Liu Y*., Hou Z.Q., 2017. A synthesis of mineralization styles with an integrated genetic model of carbonatite-syenite-hosted REE deposits in the Cenozoic Mianning-Dechang REE metallogenic belt, the eastern Tibetan Plateau, southwestern China. Journal of Asian Earth Sciences, 137, 35-79.  

　　4. Liu Y*., Chen Z.Y., Yang Z.S., Sun X., Zhu Z.M., Zhang Q.C., 2015a. Mineralogical and geochemical studies of brecciated ores in the Dalucao REE deposit, Sichuan Province, southwestern China. Ore Geology Reviews. 70, 613-636.  

　　5. Liu Y*., Zhang R.Q., Zhang Z.Y., Shi G.H., Zhang Q.C., Abuduwayiti M., Liu J.H., 2015c. Mineral inclusions and SHRIMP U–Pb dating of zircons from the Alamas nephrite and granodiorite: Implications for the genesis of a magnesian skarn deposit. Lithos 212-215, 128-144. 

　　  

　　唐明金，男， 1984年6月生，中国科学院广州地球化学研究所研究员，博士 

　　请奖项目：矿质气溶胶 

　　与请奖项目有关的主要学术成就与创新点：①系统研究了两百多种反应性气体的扩散系数，发现Fuller公式可以准确估算反应性气体扩散系数，为非均相反应的数值模拟提供了关键基础性数据；②准确测定了两种代表性氮氧化物与矿质气溶胶非均相反应的摄取系数，研究结果被国际纯粹与应用化学联合会收录和采纳，并被广泛应用于多个国际主流大气化学数值模式；③自主开发了一种新的气溶胶吸湿性测量方法，关键技术指标达到国际领先水平，并系统揭示了矿质气溶胶的吸湿性及非均相反应的影响。 

　　五篇代表性论著： 

　　1. Gu, W. J., Li, Y. J., Zhu, J. X., Jia, X. H., Lin, Q. H., Zhang, G. H., Ding, X., Song, W., Bi, X. H., Wang, X. M., and Tang, M. J.: Investigation of water adsorption and hygroscopicity of atmospherically relevant particles using a commercial vapor sorption analyzer, Atmos. Meas. Tech., 10, 3821-3832, 2017 

　　2. Tang, M. J., Huang, X., Lu, K. D., Ge, M. F., Li, Y. J., Cheng, P., Zhu, T., Ding, A. J., Zhang, Y. H., Gligorovski, S., Song, W., Ding, X., Bi, X. H., and Wang, X. M.: Heterogeneous reactions of mineral dust aerosol: implications for tropospheric oxidation capacity, Atmos. Chem. Phys., 17, 11727-11777, 2017 

　　3. Tang, M. J., Cziczo, D. J., and Grassian, V. H.: Interactions of Water with Mineral Dust Aerosol: Water Adsorption, Hygroscopicity, Cloud Condensation and Ice Nucleation, Chem. Rev., 116, 4205-4259, 2016 

　　4. Tang, M. J., Kalberer, M., and Cox, R. A.: Compilation and evaluation of gas phase diffusion coefficients of reactive trace gases in the atmosphere: volume 1. Inorganic compounds, Atmos. Chem. Phys., 14, 9233-9247, 2014 

　　5. Tang, M. J., Thieser, J., Schuster, G., and Crowley, J. N.: Uptake of NO3 and N2O5 to Saharan dust, ambient urban aerosol and soot: a relative rate study, Atmos. Chem. Phys., 10, 2965-2974, 2010 

　　  

　　王  瑞，男，1986年3月生，中国地质大学（北京）教授，博士 

　　请奖项目：后碰撞带岩浆作用和斑岩成矿  

　　与请奖项目有关的主要学术成就与创新点：①结合矿物岩石和地化证据率先指出高水和高氧逸度岩浆是形成巨型冈底斯后碰撞斑岩成矿带的关键控制因素；②进一步证实印度板片在东冈底斯带的高角度俯冲和撕裂引发了新生下地壳的重熔，促使了成矿作用集中在东冈底斯发生；③通过对西藏超钾质岩携带的中下地壳捕掳体的研究刻画了冈底斯带中新世壳幔相互作用过程，为理解碰撞带巨厚地壳形成和改造以及后碰撞斑岩成矿过程有重要的指示意义。 

　　五篇代表性论著： 

　　1. Hou, Z.Q#, Wang, R#, 2019. Fingerprinting metal transfer from mantle, Nature Communications, v10, p. 1–3.  

　　2. Wang, R#., Weinberg, R.F., Collins, W.J., Richards, J.P., Zhu, D.C., 2018. Origin of post-collisional magmas and formation of porphyry Cu deposits in southern Tibet, Earth-Science Reviews, 181, 122–143. 

　　 3. Wang, R#., Jeon, H., Evans, N., 2018, Archaean hydrothermal fluid modified zircons at Sunrise Dam and Kanowna Belle gold deposits, Western Australia: Implications for post-magmatic fluid activity and ore genesis: American Mineralogist, v. 103, p. 1891–1905 

　　4. Wang, R#., Cudahy, T., Laukamp, C., Walshe, J.L., Bath, A., Mei, Y., Young, C., Roache, T.J., Jenkins, A., Clarke, F., Baker, A., Roberts, M., and Laid, J., 2017, White mica as a hyperspectral tool in exploration for Sunrise Dam and Kanowna Belle gold deposits, Western Australia: Economic Geology, v. 112 (5), p. 1153–1176. 

　　5. Wang, R#., Richards, J.P., Hou, Z.Q., Yang, Z.M., and DuFrane, S.A., 2014, Increased magmatic water content–the key to Oligo-Miocene porphyry Cu-Mo±Au formation in the eastern Gangdese belt, Tibet: Economic Geology, v. 195 (5), p. 1315–1339.