中国矿物岩石地球化学学会第19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2023年2月17日在北京召开了评审会。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》，评选结果进行了为期10天的公示（公示时间：2023年3月1日至2023年3月10日），现公示期满，评选结果生效。公告如下（以姓氏汉语拼音排序）。柏中杰，男，1983年6月生，中国科学院地球化学研究所研究员，博士
请奖项目：幔源基性岩浆成矿作用
与请奖项目有关的主要学术成就与创新点：①发现峨眉山大火成岩省地幔源区氧逸度的不均一性，揭示成矿母岩浆继承自地幔源区的高氧逸度而非母岩浆铁钛的预富集，是磁铁矿在岩浆房中更早饱和、富集并形成世界级钒钛磁铁矿矿床的关键；②建立了沿岩浆通道脉动式补给氧化性岩浆而在较小镁铁–超镁铁层状岩体中形成超大型钒钛磁铁矿矿床的岩浆通道成矿模式，揭示了形成巨厚钒钛磁铁矿矿层的动力学机制；③初步揭示了攀西层状岩体和华南弧岩浆演化早期硫化物饱和历史及其对成矿潜力的制约，为理解岩浆（热液）矿床成因提供了新视角。五篇代表性论著：
1.Bai Z J*, Zhong H, Hu R Z, Zhu W G. 2021. World-Class Fe-Ti-V Oxide Deposits Formed in Feeder Conduits by Removing Cotectic Silicates. Economic Geology, 116(3): 681-6912.Bai Z J*, Zhong H, Hu R Z, Zhu W G. 2020. Early sulfide saturation in arc volcanic rocks of southeast China: Implications for the formation of co-magmatic porphyry–epithermal Cu–Au deposits. Geochimica et Cosmochimica Acta, 280: 66-843.Bai Z J*, Zhong H, Hu R Z, Zhu W G, Hu WJ. 2019. Composition of the Chilled Marginal Rocks of the Panzhihua Layered Intrusion, Emeishan Large Igneous Province, SW China: Implications for Parental Magma Compositions, Sulfide Saturation History and Fe–Ti Oxide Mineralization. Journal of Petrology, 60(3): 619-6484.Bai Z J, Zhong H, Li C, Zhu W G, He D F, Qi L. 2014. Contrasting Parental Magma Compositions For The Hongge And Panzhihua Magmatic Fe-Ti-V Oxide Deposits, Emeishan Large Igneous Province, Sw China. Economic Geology, 109: 1763-17855.Bai Z J, Zhong H*, Naldrett A J, Zhu W G, Xu G W. 2012. Whole-Rock and Mineral Composition Constraints on the Genesis of the Giant Hongge Fe-Ti-V Oxide Deposit in the Emeishan Large Igneous Province, Southwest China. Economic Geology, 107: 507-524龚承林，男，1983年1月生，中国石油大学（北京）教授，博士
请奖项目：深水沉积学
与请奖项目有关的主要学术成就与创新点：致力于深海沉积过程及其资源效应的深水沉积学研究，在深海沉积过程和深水源汇系统方面取得系列创新成果。针对深海沉积过程：揭示了重力流与底流相互作用的沉积模式，突破了深海沉积过程的沉积机制，开拓了深海油气勘探新领域。针对深水源汇系统：揭示了深水源汇系统的过程响应与驱动机制，提出了陆架边缘多元耦合控砂机制，建立了深水储层预测新方法。五篇代表性论著：
1.Gong C, Wang Y, Zhu W, Li W, Xu Q. 2013. Upper Miocene to Quaternary unidirectionally migrating deep-water channels in the Pearl River Mouth Basin, northern South China Sea. AAPG Bulletin, 97: 285-3082.Gong C, Wang Y, Steel R J, Peakall J, Zhao X, Sun Q. 2016. Flow processes and sedimentation in unidirectionally migrating deep-water channels: From a 3D seismic perspective. Sedimentology, 63:645–663.Gong C, Steel R J, Wang Y, Lin C, Olariu C. 2016. Shelf-margin architecture variability and its role in sediment-budget partitioning into deep-water areas. Earth-Science Reviews, 154: 72–1014.Gong C, Wang Y, Rebesco M, Salon S, Steel R J. 2018. How do turbidity flows interact with contour currents in unidirectionally migrating deep-water channels? Geology, 46: 551–5545.龚承林，王英民. 2022. 深海重力流与底流交互作用.北京：科学出版社，1-240何宇，男，1985年5月生，中国科学院地球化学研究所研究员，博士
请奖项目：地球内部超离子态物质新发现
与请奖项目有关的主要学术成就与创新点：①提出含水橄榄石中质子的热解离输运机理，从原子尺度解释了含水橄榄石的高导电性和电导率各向异性，其各向异性的高电导率可以为软流圈顶部的高导异常提供解释；②理论预测了下地幔含水矿物高压相（py-FeO2H）的超离子态转变，后被高温高压实验证实，其中快速扩散的质子使其电导率接近金属，为水在下地幔的分布提供重要的示踪作用，这对认知地球深部水循环至关重要；③发现地球内核超离子态铁-轻元素（碳、氢、氧）合金，表明内核由固态铁与快速扩散的轻元素组成，颠覆了内核是固态的传统认知，流动的轻元素导致弹性软化，解释了内核密度亏损和低横波波速之谜；④相关研究结果表明超离子态存在于地球内部，是地球科学研究中有别于气态、液态、固态和超临界态的第五种物质形态，其特殊的性质为解开地球内部运行机制等重要科学问题提供了关键线索。五篇代表性论著：
1.He Y*, Sun S C*, Kim D Y, Jang B G, Li H P, Mao H K. 2022. Superionic iron alloys and their seismic velocities in Earth’s inner core. Nature, 602: 258–2622.He Y *, Dai L D, Kim D Y, Li H P, Karato S I. 2021. Thermal Ionization of Hydrogen in Hydrous Olivine With Enhanced and Anisotropic Conductivity. Journal of Geophysical Research: Solid Earth, 126, e2021JB0229393.He Yu*, Sun S C, Li H P. 2021. Ab initio molecular dynamics investigation of the elastic properties of superionic Li2O under high temperature and pressure. Phys. Rev. B., 103:1741054.Hou M Q*, He Yu*, Jang B G, Sun S C, Zhuang Y K, Deng L W, Tang R, Chen J H, Ke F, Meng Y, Prakapenka V B, Chen B, Shim J H, Liu J, Kim D Y, Hu Q Y, Pickard C J, Needs R J, Mao H K. 2021. Superionic iron oxide–hydroxide in Earth’s deep mantle. Nature Geoscience, 14: 174-1785.Huang Y W*, He Y*, Sheng H, Lu X, Dong H N, Samanta S, Dong H L, Li X F, Kim D Y, Mao H K, Liu Y Z, Li H P, Li H, Wang L*. 2019. Li-ion battery material under high pressure: amorphization and enhanced conductivity of Li4Ti5O12. National Science Review, 6:239-246胡清扬，男，1987年4月生，北京高压科学研究中心研究员，博士
请奖项目：地球深部水与矿物的化学作用与物质循环
与请奖项目有关的主要学术成就与创新点：①形成对深地水循环的系统性认识；②提出地球深部造氧假说，揭示深地水循环的运行机制和大气演化历史；③完善高温高压下含水矿物的特性研究，革新深地水循环探测技术。五篇代表性论著：
1.Hu Q, Kim D Y, Yang W, Yang L, Meng Y, Zhang L, Mao H K*. 2016. FeO2 and FeOOH under deep lower-mantle conditions and Earth’s oxygen–hydrogen cycles. Nature, 531: 241-2442.Hu Q, Kim D Y, Liu J, Meng Y, Yang L, Zhang D, Mao W, Mao H K. 2017, Dehydrogenation of goethite in Earth’s deep lower mantle. Proceedings of the National Academy of Sciences of the U.S.A. 114: 1498-15013.Hu Q, Liu J*, Chen J, Yan B, Meng Y, Prakapenka V B, Mao W L, Mao H K*. 2021. Mineralogy of the deep lower mantle in the presence of H2O. National Science Review, 8, nwaa0984.Hou M, He Y, Jang B G, Sun S, Zhuang Y, Deng L, Tang R, Chen J, Ke F, Meng Y, Prakapenka V B, Chen,B, Shim J H, Liu J*, Kim D K*, Hu Q*, Pickard C J, Needs R J, Mao H K. 2021. Superionic iron oxide–hydroxide in Earth’s deep mantle. Nature Geoscience, 14:174-1785.Zhuang Y, Gan B, Cui Z, Tang R, Tao R, Hou M, Gang J, Catalin P, Gaston G, Zhang Y*, Hu Q*. 2022. Mid-mantle water transportation implied by the electrical and seismic properties of ε-FeOOH. Science Bulletin, 67:748-754胡森，男，1983年11月生，中国科学院地质与地球物理研究所研究员，博士
请奖项目：月球和火星的水和挥发分研究
与请奖项目有关的主要学术成就与创新点：①以科学为牵引，研发了微区水和挥发分含量及其同位素组成的分析技术，支撑了月球和火星水等重大科学问题的研究；②开展月球探测的科学研究，厘清嫦娥五号玄武岩来自一个“干”月幔，排除了月幔源区富水更易熔融维持月球年轻火山活动的猜想，为揭示月球年轻玄武岩及成因提供重要约束；③系统开展火星陨石的水含量与H同位素研究，发现火星大气降水扩散进入岩石的地化证据，证实火星2亿年仍存在过地下水活动；初步建立火星16亿年以来的古环境演化框架；揭示火幔的水、氯、硫等挥发分含量。
五篇代表性论著：
1.Hu S, Lin Y, Zhang J, Hao J, Yang W, Deng L. 2015. Measurements of water content and D/H ratio in apatite and silicate glasses using a NanoSIMS 50L. Journal of Analytical Atomic Spectrometry, 30: 967-9782.Hu S, He H, Ji J, Lin Y, Hui H, Anand M, Tartese R, Yan Y, Hao J, Li R, Gu L, Guo Q, He H, Ouyang Z. 2021. A dry lunar mantle reservoir for young mare basalts of Chang'e-5. Nature, 600: 49-533. Ji J, He H, Hu S*, Lin Y, Hui H*, Hao J, Li R, Yang W, Yan Y, Tian H, Zhang C, Anand M, Tartèse R, Gu L, Li J, Zhang D, Mao Q, Jia L, Chen Y, Wu S, Wang H, He H, Li X, Wu F. 2022. Magmatic chlorine isotope fractionation recorded in apatite from Chang'e-5 basalts. Earth and Planetary Science Letters, 591: 1176364.Hu S, Lin Y, Zhang J, Hao J, Yamaguchi A, Zhang T, Yang W, Changela H. 2020. Volatiles in the martian crust and mantle: Clues from the NWA 6162 shergottite. Earth and Planetary Science Letters, 530: 1159025.Hu S, Lin Y, Zhang J, Hao J, Feng L, Xu L, Yang W, Yang J. 2014. NanoSIMS analyses of apatite and melt inclusions in the GRV 020090 Martian meteorite: Hydrogen isotope evidence for recent past underground hydrothermal activity on Mars. Geochimica et Cosmochimica Acta, 140: 321-333李继磊，男，1984年11月生，中国科学院地质与地球物理研究所研究员，博士
请奖项目：俯冲带变质作用与元素循环
与请奖项目有关的主要学术成就与创新点：①率先通过碳酸盐矿物环带追溯俯冲带变质演化历史，揭示了俯冲带碳酸盐矿物变质演化序列，对理解俯冲带含碳相演化和深部碳循环具有重要意义；②通过榴辉岩多期变质作用揭示了俯冲隧道内多期俯冲-折返循环与隧道环流，并提出了西南天山洋壳榴辉岩的“沉积岩型”俯冲隧道折返模式；③深入揭示了俯冲带中硫的地球化学行为，查明了俯冲板片硫的赋存状态及同位素信息、板片流体中硫的溶解度及迁移行为，首次从板片角度直接全面定量地解析了俯冲带硫循环，加深了对地球“深部硫循环”体系的整体理论认知。五篇代表性论著：
1.Li J L, Schwarzenbach E M, John T, Ague J J, Huang F, Gao J, Klemd R, Whitehouse M J, Wang X S. 2020. Uncovering and quantifying the subduction zone sulfur cycle from the slab perspective. Nature Communications, 11: 5142.Li J L, Klemd R, Gao J, Meyer M. 2014. Compositional zoning in dolomite from lawsonite-bearing eclogite (SW Tianshan, China): Evidence for prograde metamorphism during subduction of oceanic crust. American Mineralogist, 99: 206-2173.Li J L, Schwarzenbach E M, John T, Ague J J, Tassara S, Gao J, Konecke B. 2021. Subduction zone sulfur mobilization and redistribution by intraslab fluid-rock interaction. Geochimica et Cosmochimica Acta, 297: 40-644.Li J L, Gao J, John T, Klemd R, Su W. 2013. Fluid-mediated metal transport in subduction zones and its link to arc-related giant ore deposits: Constraints from a sulfide- bearing HP vein in lawsonite eclogite (Tianshan, China). Geochimica et Cosmochimica Acta, 120: 326-3625.Li J L, Klemd R, Gao J, John T. 2016. Poly-cyclic metamorphic evolution of eclogite: evidence for multistage burial-exhumation cycling in a subduction channel. Journal of Petrology, 57: 119-146李舢，男，1983年4月生，中国科学院大学教授，博士
请奖项目：岩浆作用、造山过程与大陆增生
与请奖项目有关的主要学术成就与创新点：①发现同期不同“类型”花岗岩物源中均含沉积物，建立后碰撞花岗岩类多样性的成因模式；②厘定中亚增生造山带古大洋闭合期间碰撞型花岗岩，为解剖岩浆作用与造山过程的内在关联提供研究范例；③发现东南亚特提斯花岗岩中的三期新生地壳物质，提出后撤型增生造山造成地壳幕式增生的形成模型。五篇代表性论著：
1.Li S, Miller C F, Tao W, Xiao W, Chew D. 2022. Role of sediment in generating contemporaneous, diverse “type” granitoid magmas. Geology, 50: 427-4312.Li S, Chung S L, Lai Y M, Ghani A A, Lee H Y, Murtadha S. 2020. Mesozoic juvenile crustal formation in the easternmost Tethys: Zircon Hf isotopic evidence from Sumatran granitoids, Indonesia. Geology, 48: 1002-10053.Li S, Chung S L, Hou Z, Chew D, Wang T, Wang B, Wang Y. 2019. Early Mesozoic Magmatism Within the Tibetan Plateau: Implications for the Paleo-Tethyan Tectonic Evolution and Continental Amalgamation. Tectonics, 38: 3505-35434.Li S, Chung S L, Wilde S A, Jahn B M, Xiao W J, Wang T, Guo Q Q. 2017. Early-Middle Triassic high Sr/Y granitoids in the southern Central Asian Orogenic Belt: Implications for ocean closure in accretionary orogens. Journal of Geophysical Research: Solid Earth, 122: 2291-23095.Li S, Wang T, Wilde S A, Tong Y. 2013. Evolution, source and tectonic significance of Early Mesozoic granitoid magmatism in the Central Asian Orogenic Belt (central segment). Earth-Science Reviews, 126: 206-234林莽，男，1985年11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：多硫多氧同位素地球化学与非质量分馏机理
与请奖项目有关的主要学术成就与创新点：①系统建立了多种自然样品的自然丰度硫35 同位素分析方法，为示踪太阳活动、极端气候、大气物理和化学、冰川消融等空间、大气、表生环境过程提供了全新研究手段；②率先开展了五硫同位素综合研究，结合实验模拟，指出同位素非质量分馏效应的复杂性，提出了被前人忽略的同位素分馏过程，对进一步利用多硫多氧同位素研究太阳系原行星盘演化、行星表生环境和生命协同演化具有重要指示意义；③发现了青藏高原大气和沉积物硫酸盐中独特的多硫多氧同位素特征，揭示了高层大气和风化剥蚀对该地区表生环境的影响，提出了非质量分馏信号可作为古高度重建的潜在指标。五篇代表性论著：
1.Lin M*, Thiemens M H. 2022. Cosmogenic radiosulfur tracking of solar activity and the strong and long-lasting El Ni？o events. Proceedings of the National Academy of Sciences of the United States of America, 119(19): e2121550119 (封面论文)2.Lin M*, Wang K, Kang S, Li Y, Fan Z, Thiemens M H. 2021. Isotopic signatures of stratospheric air at the Himalayas and beyond. Science Bulletin, 66(4): 323-3263.Lin M*, Zhang X, Li M, Xu Y, Zhang Z, Tao J, Su B, Liu L, Shen Y*, Thiemens M H*. 2018. Five-S-isotope evidence of two distinct mass-independent sulfur isotope effects and implications for the modern and Archean atmospheres. Proceedings of the National Academy of Sciences of the United States of America, 115 (34): 8541-85464.Lin M*, Kang S, Shaheen R, Li C, Hsu S C, Thiemens M H*. 2018. Atmospheric sulfur isotopic anomalies recorded at Mt. Everest across the Anthropocene. Proceedings of the National Academy of Sciences of the United States of America, 115(27): 6964-69695.Lin M*, Su L, Shaheen R, Fung J C H, Thiemens M H*. 2016. Detection of deep stratospheric intrusions by cosmogenic 35S. Proceedings of the National Academy of Sciences of the United States of America, 113(40): 11131-11136刘平平，女，1986年11月生，北京大学助理教授，博士
请奖项目：岩浆深部过程与资源环境效应
与请奖项目有关的主要学术成就与创新点：①限定了多巴火山超级喷发前浅部岩浆房的岩浆注入速率，提出持续而稳定的岩浆注入可以导致超级喷发，短时间内大量岩浆注入不是超级喷发的必要条件；②厘定了大洋地幔储库的镁同位素组成，系统阐述了深海橄榄岩镁和锂同位素的分馏机制，并制约了超慢速扩张洋中脊地幔岩的冷却速率；③开展基性-超基性层状侵入体微区结构、三维层析成像和非传统稳定同位素地球化学研究，揭示了含钒钛磁铁矿基性-超基性层状侵入体的岩浆不混熔过程及其镁铁同位素分馏机理。五篇代表性论著：
1.Liu P P, Caricchi L, Chung S L, Li X H, Li Q L, Zhou M F, Lai Y M, Ghani A A, Sihotang T, Sheldrake T E. 2021. Growth and thermal maturation of the Toba magma reservoir. Proceedings of the National Academy of Sciences, 118: e21016951182.Liu P P, Chung S L, Chesner C A, Gao M H, Lai Y M, Lee H Y, Yang Y H. 2022. New Insights Into the Petrogenesis of Voluminous Crustal-Signature Silicic Volcanic Rocks of the Toba Eruptions (Indonesia). Journal of Geophysical Research: Solid Earth, 127: e2022JB0245593.Liu P P, Liang J, Dick H J B, Li X H, Chen Q, Zuo H Y, Wu J C. 2020. Enormous Lithium Isotopic Variations of Abyssal Peridotites Reveal Fast Cooling and Melt/Fluid-Rock Interactions. Journal of Geophysical Research: Solid Earth, 125: e2020JB0203934.Liu P P, Teng F Z, Dick H J B, Zhou M F, Chung S L. 2017. Magnesium isotopic composition of the oceanic mantle and oceanic Mg cycling. Geochimica Et Cosmochimica Acta, 206: 151-1655.Liu P P, Zhou M F, Luais B, Cividini D, Rollion-Bard C. 2014. Disequilibrium iron isotopic fractionation during the high-temperature magmatic differentiation of the Baima Fe-Ti oxide-bearing mafic intrusion, SW China. Earth and Planetary Science Letters, 399: 21-29罗根明，男，1984年8月生，中国地质大学（武汉）教授，博士
请奖项目：重大地质转折期生物与环境相互作用与协同演化
与请奖项目有关的主要学术成就与创新点：①从硫-碳循环角度限定了大气氧含量在元古宙早期的变化过程与时间框架，建立了氮循环从无氧体系向有氧体系转变的关键过程；②全面而系统地揭示了二叠纪-三叠纪之交地质微生物参与的碳、氮、硫循环过程，修正了古海洋水化学的传统认识，提出了微生物地质过程促发的温室气体释放通量升高的新观点。五篇代表性论著（#共同第一作者，*通讯作者）：
1.Izon G*, Luo G M*, Uveges B T, Beukes N, Kitajima K, Ono S, Valley J W, Ma X Y, Summons R E*. 2022. Bulk and grain-scale minor sulfur isotope data reveal complexities in the dynamics of Earth’s oxygenation. Proceedings of the National Academy of Science, USA, 119: e20256061192.Luo G M*, Junium C K, Izon G, Ono S, Beukes N J, Algeo T J, Cui Y, Xie S, Summons R E*. 2018. Nitrogen fixation sustained productivity in the wake of the Palaeoproterozoic Great Oxygenation Event. Nature Communications, 9:9783.Luo G M*, Ono S, Beukes N J, Wang D T, Xie S C, Summons R E*. 2016. Rapid oxygenation of Earth’s atmosphere 2.33 billion years ago. Science Advances, 2: e16001344.Luo G M, Wang Y, Algeo T J, Kump L R, Bai X, Yang H, Yao L, Xie S*. 2011. Enhanced nitrogen fixation in the immediate aftermath of the latest Permian marine mass extinction. Geology, 39: 647-6505.Luo G M, Kump L R, Wang Y B, Tong J N, Arthur M A, Yang H, Huang J H, Yin H F, Xie S C*. 2010. Isotopic evidence for an anomalously low oceanic sulphate concentration following end-Permian mass extinction. Earth and Planetary Science Letters, 300: 101-111马强，男，1985年11月生，中国地质大学（武汉）教授，博士
请奖项目：岩浆过程与大陆演化
与请奖项目有关的主要学术成就与创新点：①揭示了华北克拉通深部地壳的属性，厘定了38亿年的下地壳岩石，为中国东部大陆地壳的形成演化和圈层相互作用提供了制约；②提出了大陆埃达克质岩浆岩新的成因模式，约束了晚中生代时期华北克拉通的地壳厚度，论证了华北克拉通自下而上的破坏过程；③发现了华北中生代岩浆迁移规律，提出东亚大地幔楔系统最初形成于早白垩世，为华北克拉通破坏与古太平洋板块俯冲的关联提供了关键证据。五篇代表性论著：
1.Ma Q, Zheng J P, Xu Y G, Griffin W L, Zhang R S. 2015. Are continental “adakites” derived from thickened or foundered lower crust? Earth and Planetary Science Letters, 419:125-1332.Ma Q, Xu Y G. 2021. Magmatic perspective on subduction of Paleo-Pacific plate and initiation of big mantle wedge in East Asia. Earth-Science Reviews, 213:103-4733.Ma Q, Xu Y G, Huang X L, Zheng J P, Ping X, Xia X P. 2020. Eoarchean to Paleoproterozoic crustal evolution in the North China Craton: Evidence from U-Pb and Hf-O isotopes of zircons from deep-crustal xenoliths. Geochimica et Cosmochimica Acta, 278: 94-1094.Ma Q, Xu Y G, Zheng J P, Griffin W L, Hong L B, Ma L. 2016. Coexisting Early Cretaceous High-Mg Andesites and Adakitic Rocks in the North China Craton: the Role of Water in Intraplate Magmatism and Cratonic Destruction. Journal of Petrology, 57(7):1279-13085.Ma Q, Zheng J P, Griffin W L, Zhang M, Tang H Y, Su Y P, Ping X Q. 2012. Triassic “adakitic” rocks in an extensional setting (North China): Melts from the cratonic lower crust. Lithos, 149: 159-173欧阳荷根，男，1984年10月生，中国地质科学院矿产资源研究所研究员，博士
请奖项目：大型-超大型岩浆-热液矿床的形成机制：以钼矿为例
与请奖项目有关的主要学术成就与创新点：①发现不同构造环境的成钼矿岩浆均不富钼，提出氧化性富水岩浆是形成斑岩-矽卡岩型钼矿的基础，成矿流体沿岩浆房顶部衍生的小岩株高度聚集是成矿之关键环节；②定量化揭示出大型-超大型斑岩-矽卡岩型钼矿的多期次成矿特点，提出大型-超大型钼矿形成的关键因素是成矿岩体与大岩浆房相连，且含矿岩浆多期侵位与成矿；③揭示出成矿岩浆的硫和氯含量是制约斑岩矿床形成钼矿化或铜钼矿化的重要因素，提出岩浆成因磷灰石的硫和氯可用来识别不成矿、成钼矿和成铜钼矿岩体之新认识。五篇代表性论著：
1.Ouyang H G*, Caulfield J. 2022. Understanding Cu deficiency and Mo enrichment in the Jurassic Zhangguangcai-Lesser Xing’an continental-arc (NE China): Insights from the Luming porphyry Mo deposit. Economic Geology, doi:10.5382/econgeo.4989
2.Ouyang H G*, Gaynor S P, Selby D, Mao J W, Shu Q H, Li C. 2022. High-precision geochronology of the Xiaojiayingzi Mo skarn deposit: Implications for prolonged and episodic hydrothermal pulses. Economic Geology, doi:10.5382/econgeo.4984
3.Ouyang H G*, Caulfield J, Mao J W, Hu R Z. 2022. Controls on the formation of porphyry Mo deposits: Insights from porphyry (-skarn) Mo deposits in northeastern China. American Mineralogist, 107: 1736-1751
4.Ouyang H G*, Mao J W, Hu R Z, Caulfield J, Zhou Z H. 2021. Controls on the metal endowment of porphyry Mo deposits: insights from the Luming porphyry Mo deposit, northeastern China. Economic Geology, 116: 1711-1735
5.Ouyang H G*, Mao J W, Hu R Z. 2020. Geochemistry and Crystallization Conditions of Magmas Related to Porphyry Mo Mineralization in Northeastern China. Economic Geology, 115: 79-100
孙若愚，男，1986年8月生，天津大学教授，博士
请奖项目：汞同位素环境地球化学
与请奖项目有关的主要学术成就与创新点：①认清了世界煤炭汞同位素变化特征，提出了燃煤过程汞同位素分馏模型，并构建了工业革命以来燃煤汞排放的同位素演变历史；②建立了人为和自然源汞排放的同位素数据库，构建了基于汞同位素的全球汞循环模型；③初步认清了海洋汞循环的基本规律，率先发现全球最深海洋马里亚纳海沟生物中的汞来自于上层海洋的人为源甲基汞。五篇代表性论著：
1.Sun R Y, Yuan J J, Sonke J E, Zhang Y X, Zhang T, Zheng W, Chen S, Meng M, Chen J B, Liu Y*, Peng X T*,Liu C Q. 2020. Methylmercury produced in upper oceans accumulates in deep Mariana Trench fauna. Nature Communications, 11(1): 33892.Sun R Y*, Jiskra M, Amos H M, Zhang Y X, Sunderland E M, Sonke J E*. 2019. Modelling the mercury stable isotope distribution of Earth surface reservoirs: Implications for global Hg cycling. Geochimica et Cosmochimica Acta, 246: 156-1733.Sun R Y*, Sonke J E, Liu G J. 2016. Biogeochemical controls on mercury stable isotope compositions of world coal deposits: A review. Earth-Science Reviews, 152: 1-134.Sun R Y, Hintelmann H, Liu Y*, Li X H, Dimock B. 2016. Two Centuries of Coral Skeletons from the Northern South China Sea Record Mercury Emissions from Modern Chinese Wars. Environmental Science & Technology, 50(11): 5481-54885.Sun R Y*, Sonke J E*, Heimbürger L E, Belkin H E, Liu G J, Shome D, Cukrowska E, Liousse C, Pokrovsky O S, Streets D G. 2014. Mercury Stable Isotope Signatures of World Coal Deposits and Historical Coal Combustion Emissions. Environmental Science & Technology, 48(13): 7660-7668汪在聪，男，1985年9月生，中国地质大学（武汉）教授，博士
请奖项目：行星早期增生与壳幔演化
与请奖项目有关的主要学术成就与创新点：①建立高精度方法获得了硅酸盐地球中多种亲铁元素的准确丰度值，创新地论述了地球不同增生阶段的挥发性元素组成，为地球上水的起源以及地球增生物质的模型提供关键约束；②提出火星内部并不富含硫和火星水起源于核幔分异之前等革新性认识，改变了过去广泛认为火星内部富含硫的传统观点，极大丰富了对地球和火星早期增生演化与宜居条件形成的认识；③建立铜银比值新指标揭示了地壳深部硫化物堆晶和拆沉是壳幔分异的重要环节；开发高精度金含量分析方法阐明了华北克拉通壳幔长期演化控制巨量金成矿机制，揭示出交代地幔源区无需强烈富集金也能形成超大型金成矿省。五篇代表性论著：
1.Wang Z C, Becker Harry.2013. Ratios of S, Se and Te in the silicate Earth require a volatile-rich late veneer. Nature, 499: 328-3312.Wang Z C, Laurenz Vera, Petitgirard Sylvain, Becker Harry. 2016. Earth's moderately volatile element composition may not be chondritic: Evidence from In, Cd and Zn. Earth and Planetary Science Letters, 435: 136-1463.Wang Z C, Becker Harry. 2017. Chalcophile elements in Martian meteorites indicate low sulfur content in the Martian interior and a volatile element-depleted late veneer. Earth and Planetary Science Letters, 463: 56-684.Wang Z C, Becker Harry, Liu Y S, Hoffmann Elis, Chen C F, Zou Z Q, Li Y. 2018. Constant Cu/Ag in upper mantle and oceanic crust: Implications for the role of cumulates during the formation of continental crust. Earth and Planetary Science Letters, 493: 25-355.Wang Z C, Cheng H, Zong K Q, Geng X L, Liu Y S, Yang J H, Wu F Y, Becker Harry, Foley Stephen, Wang, Christina Yan. 2020. Metasomatized lithospheric mantle for Mesozoic giant gold deposits in the North China craton. Geology, 48:169-173王华建，男，1984年9月生，中国石油勘探开发研究院高级工程师，博士
请奖项目：有机质富集生烃的多元相互作用
与请奖项目有关的主要学术成就与创新点：①证实了深部动力活动和铁输入通量控制中元古代有机质富集程度和生烃潜力，提出中国华北中元古界具有页岩油气勘探前景；②利用微束多元素成像技术明确了多种“矿物探针”成因，揭示了有机质矿化的微生物作用和古水体的动态演化过程；③设计实施了首例核反应堆中子辐照生烃模拟实验，提出放射性作用导致有机质演化生烃的新模式，补充了富铀烃源岩的资源潜力评价参数。五篇代表性论著：
1.Wang H J, Ye Y T, Deng Y, Wang X M, Hammarlund E U, Fan H F, Canfield D E*, Zhang S C*. 2022. Isotope evidence for the coupled iron and carbon cycles 1.4 billion years ago. Geochemical Perspectives Letters, 21: 1-62.Deng Y, Wang H J*, Lyu D, Zhang F L, Gao Z Y, Ren R, Ye Y T, Lyu Y T, Wang X M, Guan P, Zhang S C. 2021. Evolution of the 1.8–1.6 Ga Yanliao and Xiong’er basins, north China Craton. Precambrian Research, 365: 1063833.Wang H J*, Ye Y T, Deng Y, Liu Y K, Lyu Y T, Zhang F L, Wang X M, Zhang S C. 2021. Multi-element imaging of a 1.4 Ga authigenic siderite crystal. Minerals, 11(12): 13954.Zhang F L, Wang H J*, Ye Y T, Deng Y, Lyu Y T, Wang X M, Yu Z C, Lyu D, Lu Y Z, Zhou C M, Bi L, Deng S H, Zhang S C, Canfield D E. 2021. The environmental context of carbonaceous compressions and implications for organism preservation 1.40 Ga and 0.63 Ga. Palaeogeography, Palaeoclimatology, Palaeoecology, 573: 1104495.Wang H J*, Zhao W Z, Cai Y W, Wang X M, Ye Y T, Su J, He K, Zhang W L, Huang L, Zhang S C. 2020. Oil generation from the immature organic matter after artificial neutron irradiation. Energy & Fuels, 34(2): 1276-1287王煜，男，1985年2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：再循环地壳组分在地幔中的熔融行为
与请奖项目有关的主要学术成就与创新点：①揭示了再循环下洋壳和陆壳在地幔中的熔融过程，为研究地幔不均一性及深部物质循环提供了精细实验岩石学依据；②阐明了再循环地壳组分对钾质-超钾质岩地幔源区的重要控制作用，为识别钾质岩源区组成及约束钾质岩浆生成和演化过程提供了关键实验约束；③发现了富集陆源成因蓝片岩在造山带钾质-超钾质岩成因中的重要作用，提出了不同于传统认识的浅俯冲成因模型。五篇代表性论著：
1.Wang Y*, Foley S F, Buhre S, Soldner J, Xu Y G. 2021. Origin of potassic postcollisional volcanic rocks in young, shallow, blueschist-rich lithosphere. Science Advances, 7: eabc02912.Wang Y*, Foley S F, Prelevi？D. 2017. Potassium-rich magmatism from a phlogopite-free source. Geology, 45:467-4703.Wang Y*, Xu Y G. 2020. Partial Melting of the Lower Oceanic Crust: Implications for Tracing the Slab Component in the Source of Mid-Ocean Ridge Basalts. Journal of Geophysical Research: Solid Earth, 125: e2020JB0206734.Wang Y*, Foley S F. 2020. The Role of Blueschist Stored in Shallow Lithosphere in the Generation of Postcollisional Orogenic Magmas. Journal of Geophysical Research: Solid Earth, 125: e2020JB0199105.Wang Y*, Foley S F. 2018. Hybridization Melting Between Continent-Derived Sediment and Depleted Peridotite in Subduction Zones. Journal of Geophysical Research: Solid Earth,123: 3414-3429魏源，男，1983年12月生，中国环境科学研究院研究员，博士
请奖项目：区域流域系统保护修复
与请奖项目有关的主要学术成就与创新点：①开展了我国多个典型地理单元山水林田湖草系统治理研究，提出了差异化的分区理论和技术路线图，支撑国家多个重大山水修复试点工程实施。②揭示了植物适应喀斯特生态环境新机制，构建了以菌根技术为核心的地下微生态-地上复层植被耦合的立体生态恢复技术体系并成功应用，为我国石漠化治理提供了新的理论支撑和生态调控模式。③突破了锑的生物地球化学循环理论瓶颈；研发了AM真菌-苎麻联合修复锑砷复合污染土壤技术并在多地成功应用，为我国复合污染土壤修复提供了新的理论基础和技术支撑。五篇代表性论著：
1.魏源 等. 2020.喀斯特地区土壤微生物多样性及与植物适生性关系研究.北京：中国环境出版集团2.魏源 等. 2021. 贺兰山东麓山水林田湖草生态保护修复案例研究. 北京：中国环境出版集团3.Xi L, Shen Y Q, Zhao X, Zhou M, Mi Y D, Li X R, Chen H Y, Wei Y*, Su H L, Hou H. 2021. Effects of arbuscular mycorrhizal fungi on frond antimony enrichment, morphology, and proteomics in Pteris cretica var. nervosa during antimony phytoremediation. The Science of the total environment, 804: 1499044.Zhou M, Li X R, Liu X S, Mi Y D, Fu Z Y, Zhang R Q, Su H L, Wei Y*, Liu H F, Wang F F. 2022. Effects of Antimony on Rice Growth and Its Existing Forms in Rice Under Arbuscular Mycorrhizal Fungi Environment. Frontiers in Microbiology, 13: 8143235.Wei Y, Dong Z M, Fan W H, Xu K Q, Tang S, Wang Y, Wu F C. 2022. A narrative review on the role of temperature and humidity in COVID-19: Transmission, persistence, and epidemiological evidence. Eco-Environment & Health, 1(2): 73-85曾罡，男，1985年8月生，南京大学副教授，博士
请奖项目：深部地幔组成与幔源岩石成因
与请奖项目有关的主要学术成就与创新点：①揭示中国东部新生代玄武岩的源区地幔发生碳酸盐化，阐明了再循环地壳物质的深部熔融机制；②通过对地幔复杂岩性的准确厘定，深入揭示了玄武岩成因的多样性，解析了地球深部物质循环机理；③提出了幔源玄武质岩浆在地球深部演化的两种新机制。五篇代表性论著：
1.Zeng G, Chen L H*, Hofmann A W, Jiang S Y, Xu X S. 2011. Crust recycling in the sources of two parallel volcanic chains in Shandong, North China. Earth Planet. Sci. Lett., 302:359-368
2.Zeng G*, He Z Y, Li Z, Xu X S, Chen L H. 2016. Geodynamics of paleo-Pacific plate subduction constrained by the source lithologies of Late Mesozoic basalts in southeastern China. Geophys. Res. Lett., 43: 10189-10197
3.Zeng G, Chen L H*, Yu X, Liu J Q, Xu X S, Erdmann S. 2017. Magma-magma interaction in the mantle beneath eastern China. J. Geophys. Res.: Solid Earth, 122: 2763-2779
4.Zeng G*, Chen L H*, Hofmann A W*, Wang X J, Liu J Q, Yu X, Xie L W. 2021. Nephelinites in eastern China originating from the mantle transition zone. Chem. Geol., 576, doi: 10.1016/j.chemgeo.2021.120276
5. Shi J H, Zeng G*, Chen L H, Hanyu T, Wang X J, Zhong Y, Xie L W, Xie W L. 2022. An eclogitic component in the Pitcairn mantle plume: evidence from olivine compositions and Fe isotopes of basalts. Geochim. Cosmochim. Acta, 318: 415-427
翟德高，男，1985年3月生，中国地质大学（北京）教授，博士
请奖项目：低温体系金银成矿
与请奖项目有关的主要学术成就与创新点：①突破了浅成低温热液矿床中流体沸腾作用导致金富集的主流观点，提出流体混合和围岩硫化作用是金和碲富集的新机制，发展了浅成低温热液金矿床成矿理论；②提出水/岩反应使体系发生还原和降温是导致银富集沉淀的关键机制，揭示了浅成低温热液型银矿床与斑岩成矿系统的内在成因联系，推动了找矿勘查；③发现了辉钼矿颗粒内部Re极度不均一分布是控制Re-Os同位素发生解耦的一种重要机制，使用该体系限定超大型岩浆热液矿床的形成具有短期瞬时的特点。五篇代表性论著：
1.Zhai D G, Williams-Jones A E, Liu J, David S, Voudouris P C, Tombros S, Li K, Li P, Sun H. 2020. The genesis of the giant Shuangjianzishan epithermal Ag-Pb-Zn deposit, Inner Mongolia, northeastern China. Economic Geology, 115(1): 101-1282.Zhai D G, Williams-Jones A E, Liu J, David S, Li C, Huang X W, Qi L, Guo D. 2019. Evaluating the use of the molybdenite Re-Os chronometer in dating gold mineralization: Evidence from the Haigou deposit, NE China. Economic Geology, 114(5): 897-9153.Zhai D G, Williams-Jones A E, Liu J, Tombros S F, Cook N J. 2018. Mineralogical, fluid inclusion and multiple isotope (H-O-S-Pb) constraints on the genesis of the Sandaowanzi epithermal Au-Ag-Te deposit, NE China. Economic Geology, 113 (6): 1359-13824.Zhai D G, Liu J, Zhang A, Sun Y. 2017. U-Pb, Re-Os and 40Ar/39Ar Geochronology of porphyry Sn ± Cu ± Mo and polymetallic (Ag-Pb-Zn-Cu) vein mineralization at Bianjiadayuan, Inner Mongolia, NE China: Implications for discrete mineralization events. Economic Geology, 112: 2041-20595.Zhai D G, Mathur R, Liu S A, Liu J, Godfrey L, Wang K, Xu J, Vervoort J. 2021. Antimony isotope fractionation in hydrothermal systems. Geochimica et Cosmochimica Acta, 306: 84-97
张艳利，女，1984年2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：表层地球系统痕量活性有机气体
与请奖项目有关的主要学术成就与创新点：①基于定点长期和大范围多点同步野外观测，揭示我国消耗臭氧层物质和痕量卤代温室气体的历史演变并估算区域排放量，支撑我国国际履约评估；②获得典型源痕量活性气体排放的分子指纹特征谱，辨识环境空气中生成O3和SOA关键前体物并定量解析其重要来源，建立基于观测的方法体系进行单一或多种措施减排实效评估；③通过外场实测约束模型模拟BVOCs不确定性，自主设计测量植物BVOCs排放的动态箱系统，基于原位实测建立本地优势树种BVOCs排放因子库，构建排放清单并量化对区域O3生成贡献。五篇代表性论著：
1.Zhang Y L, Zhang R., Yu J Z, Zhang Z, Yang W Q, Zhang H N, Lyu S J, Wang Y S, Wang Y H, Wang X M*. 2020. Isoprene mixing ratios measured at twenty sites in China during 2012-2014: comparison with model simulation. Journal of Geophysical Research: Atmospheres, 125, e2020JD033523. https://doi.org/10.1029/2020JD0335232.Zhang Z, Zhang Y L*, Wang X M, Lü S J, Huang Z H, Huang X Y, Yang W Q, Wang Y S, Zhang Q. 2016. Spatiotemporal patterns and source implication of aromatic hydrocarbons at six rural sites across China's developed coastal regions. Journal of Geophysical Research: Atmospheres, 121, 6669-6687. doi:10.1002/2016JD0251153.Zhang Y L, Guo H, Wang X M*, Simpson I J, Barletta B, Blake D R, Meinardi S, Rowland F S, Cheng H R, Saunders S M, Lam S H M. 2010. Emission patterns and spatiotemporal variations of halocarbons in the Pearl River Delta region, southern China. Journal of Geophysical Research: Atmospheres, 115, D15309, doi:10.1029/2009 JD0137264.Zhang Y L, Wang X M*, Simpson I J, Barletta B, Blake D R, Meinardi S, Louie P K K, Zhao X, Shao M, Zhong L, Wang B, Wu D. 2014. Ambient CFCs and HCFC-22 observed concurrently at 84 sites in the Pearl River Delta region during the 2008-2009 grid studies. Journal of Geophysical Research: Atmospheres, 119(12): 7699-7717. doi:10.1002/2014JD0216265.Zhang Y L, Wang X M*, Blake D R, Li L, Zhang Z, Wang S, Guo H, Lee S C, Gao B, Chan L, Wu D, Rowland F S. 2012. Aromatic hydrocarbons as ozone precursors before and after outbreak of the 2008 financial crisis in the Pearl River Delta region, south China. Journal of Geophysical Research: Atmospheres, 117, D15306, doi:10.1029/2011JD017356