第17届侯德封矿物岩石地球化学青年科学家奖评选公告
中国矿物岩石地球化学学会第17届侯德封矿物岩石地球化学青年科学家奖
评选公告
2018年4月21日，我会第九届侯德封奖评选工作委员会在合肥召开了评审会。16名评选委员会委员到会。会议由评选委员会主任刘丛强院士主持。评选委员会经过认真评审、讨论，以无记名投票方式产生了21名获奖者。
本次评选结果经本学会第九届理事会第三次常务理事（扩大）会议审议，经公示（公示时间：2018-04-25至2018-05-05）无异议，评选结果生效。现将评选结果公告如下（以姓氏汉语拼音为序）。
陈 意，男，1980年12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：板块俯冲及其改造的岩石学过程。
与请奖项目有关的主要学术成就与创新点：①率先将热力学模拟计算与岩石密度算法融合，建立俯冲洋壳密度演化曲线，首次提出洋壳榴辉岩折返的极限不超过120公里；②通过对大别-苏鲁造山带橄榄岩的研究，揭示俯冲大陆板块之上的地慢楔经历了异常复杂的变质-交代-吸水-脱水过程，为深入理解俯冲带壳幔相互作用提供了强有力的岩石学证据；③构建北大别下地壳麻粒岩早元古代和三叠纪两个构造旋回的完整变质演化过程，对重新认识大陆下地壳俯冲变质和构造演化过程有重要指示意义。
五篇代表性论著：
1.Chen Y, Su B, Chu ZY. 2017. Modification of an ancient subcontinental lithospheric mantle by continental subduction: Insight from the Maowu garnet peridotites in the Dabie UHP belt, eastern China. Lithos, 278-281: 54-71.
2.Chen Y, Ye K, Wu TF, Guo S. 2013. Exhumation of oceanic eclogites: thermodynamic constraints on pressure, temperature, bulk composition and density. Journal of Metamorphic Geology, 31: 549–570.
3.Chen Y, Ye K, Wu YW, Guo S, Su B, Liu JB. 2013. Hydration and dehydration in the lower margin of a cold mantle wedge: implications for crust–mantle interactions and petrogeneses of arc magmas. International Geology Review, 55: 1506-1522.
4.Chen Y, Ye K, Liu JB, Sun M. 2008. Quantitative P-T-X constraints on orthopyroxene-bearing high-pressure granulites in felsic-metapelitic rocks: evidence from the Huangtuling granulite, Dabieshan Orogen. Journal of Metamorphic Geology, 26: 1-15.
5.Chen Y, Ye K, Liu JB, Sun M. 2006. Multistage metamorphism of the Huangtuling granulite, Northern Dabie Orogen, eastern China: implications for the tectonometamorphic evolution of subducted lower continental crust. Journal of Metamorphic Geology, 24: 633-654.
陈仁旭，男，1981年9月生，中国科学技术大学特任教授，博士。请奖项目：大陆俯冲带流体地球化学。
与请奖项目有关的主要学术创新点：①确定了深俯冲陆壳折返过程中的流体来源和活动方式，定量厘定出经受超高压变质的地壳内部流体活动尺度，定量确定了榴辉岩和片麻岩含水性差异；②建立了不同类型新生长和重结晶锆石的地球化学判别指标，揭示出俯冲陆壳不同部位和不同岩性岩石差异性的熔流体活动行为；③发现造山带橄榄岩中锆石为地壳交代成因，揭示出这些岩石在大陆俯冲隧道受到多期次俯冲陆壳的交代作用，识别出它们受到了陆壳俯冲之前古洋壳的交代作用；④发现交代成因石榴辉石岩具有高的水含量，能提供高水含量和变化H2O/Ce比的地幔源区。
五篇代表性论著：
1.Chen RX, Li HY, Zheng YF, et al. 2017. Crust-mantle interaction in a continental subduction channel: evidence from orogenic peridotites in North Qaidam, northern Tibet. Journal of Petrology, 58: 191-226.
2.Chen RX, Zheng YF, Gong B. 2011. Mineral hydrogen isotopes and water contents in ultrahigh-pressure metabasite and metagranite: Constraints on fluid flow during continental subduction-zone metamorphism. Chemical Geology. 281: 103-124.
3.Chen RX, Zheng YF, Xie LW. 2010. Metamorphic growth and recrystallization of zircon: distinction by simultaneous in-situ analyses of trace elements, U-Th-Pb and Lu-Hf isotopes in zircon from eclogite-facies rocks in the Sulu orogen. Lithos, 114: 132-154.
4.Chen RX, Zheng YF, Gong B, et al. 2007. Oxygen isotope geochemistry of ultrahigh-pressure metamorphic rocks from 200-4000 m core samples of the Chinese Continental Scientific Drilling. Chemical Geology, 242: 55-75.
5.Chen RX, Zheng YF, Gong B, et al. 2007. Origin of retrograde fluid in ultrahigh-pressure metamorphic rocks: constraints from mineral hydrogen isotope and water content changes in eclogite-gneiss transitions in the Sulu orogen. Geochim. Cosmochim. Acta, 71: 2299-2325.
邓文峰，男，1979年3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：全新世南海-西太平洋气候变化的珊瑚地球化学记录。
与请奖项目有关的主要学术成就与创新点：①发现了南海-西太平洋中全新世季节尺度“温雨解耦”的气候特征；②揭示了近2000年以来南海-西太平洋年代际-百年尺度气候变化对区域及全球气候变化的响应机制；③系统研究了珊瑚碳、钙同位素体系对气候环境变化和生物活动的响应机理，拓展了潜在的生物活动替代指标；④首次建立了激光剥蚀-等离子体光谱联机的珊瑚原位元素比值分析方法。
五篇代表性论著：
1.Deng WF, Chen XF, Wei GJ, et al. 2017. Decoupling of coral skeletal δ13C and solar irradiance over the past millennium caused by the oceanic Suess effect. Paleoceanography, 32: 161-171.
2.Deng WF, Liu X, Chen XF, et al. 2017. A comparison of the climates of the Medieval Climate Anomaly, Little Ice Age, and Current Warm Period reconstructed using coral records from the northern South China Sea. Journal of Geophysical Research: Oceans, 121: 264-275.
3.Deng WF, Wei GJ, Yu KF, Zhao JX. 2014. Variations in the timing of the rainy season in the northern South China Sea during the middle to late Holocene. Paleoceanography, 29: 115-125.
4.Deng WF, Wei GJ, Xie LH, et al. 2013. Variations in the Pacific Decadal Oscillation since 1853 in a coral record from the northern South China Sea. Journal of Geophysical Research: Oceans, 118: 2358-2366.
5.Deng WF, Liu Y, Wei GJ, et al. 2010. High-precision analysis of Sr/Ca and Mg/Ca ratios in corals by laser ablation inductively coupled plasma optical emission spectrometry. Journal of Analytical Atomic Spectrometry, 25: 84-87.
冯 东，男，1980年10月生，中国科学院南海海洋研究所研究员，博士。请奖项目：海底冷泉沉积地球化学研究。
与请奖项目有关的主要学术成就与创新点：①揭示了海底冷泉系统流体渗漏速率控制硫酸盐还原速率，发现了地质历史时期富甲烷环境自生碳酸盐岩均具有独特的晶格硫δ18O/δ34S斜率；②确定了海底冷泉流体渗漏活动主要在低海平面或海平面下降时期发育，开展了我国活动冷泉原位深潜观察和研究；③发现了冷泉系统流体活动的动态性，揭示了冷泉碳酸盐岩中微量元素富集机制；④发现了冷泉双壳类化能自养过程的稳定同位素“指纹”记录。
五篇代表性论著：
1.Feng D, Peckmann J, Li N, et al. 2018. The stable isotope fingerprint of chemosymbiosis in the shell organic matrix of seep-dwelling bivalves. Chemical Geology, 479: 241-250.
2.Feng D, Peng Y, Bao H, et al. 2016. A carbonate-based proxy for sulfate-driven anaerobic oxidation of methane. Geology, 44: 999-1002.
3.Feng D, Birgel D, Peckmann J, et al. 2014. Time integrated variation of sources of fluids and seepage dynamics archived in authigenic carbonates from Gulf of Mexico Gas Hydrate Seafloor Observatory. Chemical Geology, 385: 129-139.
4.Feng D, Roberts HH. 2011. Geochemical characteristics of the barite deposits at cold seeps from the northern Gulf of Mexico continental slope. Earth and Planetary Science Letters, 309: 89-99.
5.Birgel D, Feng D, Roberts HH, Peckmann J. 2011. Changing redox conditions at cold seeps as revealed by authigenic carbonates from Alaminos Canyon, northern Gulf of Mexico. Chemical Geology, 285: 82-96.
高晓英，女，1980年4月生，中国科学技术大学特任教授，博士。请奖项目：大陆俯冲带变质矿物学。
与请奖项目有关的主要学术成就与创新点：①识别出矿物多期次变质生长，厘定出俯冲带完整连续的P-T-t演化轨迹，揭示出深俯冲陆壳的多阶段变质演化过程；②识别出大陆俯冲带硅酸盐和碳酸盐熔体的存在，建立了大束斑外剥和小束斑内剥法，定量计算并获得熔体包体的微量元素组成，进而限定初始熔体的组成、时限以及熔融机制和演化过程；③通过对超高压变质岩中副矿物的微区原位研究，示踪大陆俯冲带熔/流体活动过程中高场强元素迁移的过程和机制。
五篇代表性论著：
1.Gao XY, Zheng YF, Chen YX, Tang HL, Li WC. 2015. Zircon geochemistry records the action of metamorphic fluid on the formation of ultrahigh-pressure jadeite quartzite in the Dabie orogen. Chemical Geology, 419: 158-175.
2.Gao XY, Zheng YF, Xia XP, Chen YX. 2014. U-Pb ages and trace elements of metamorphic rutile from ultrahigh-pressure quartzite in the Sulu orogen. Geochimica et Cosmochimica Acta, 143: 87-114.
3.Gao XY, Zheng YF, Chen YX. 2013. Trace element composition of continentally subducted slab-derived melt: insight from multiphase solid inclusions in ultrahigh-pressure eclogite in the Dabie orogen. Journal of Metamorphic Geology, 31: 453-468.
4.Gao XY, Zheng YF, Chen YX. 2012. Dehydration melting of ultrahigh-pressure eclogite in the Dabie orogen: evidence from multiphase solid inclusions in garnet. Journal of Metamorphic Geology, 30: 193-212.
5.Gao XY, Zheng YF, Chen YX. 2011. U-Pb ages and trace elements in metamorphic zircon and titanite from UHP eclogite in the Dabie orogen: constraints on P-T-t path. Journal of Metamorphic Geology, 29: 721-740.
黄汝锦，男，1979年12月生，中国科学院地球环境研究所研究员，博士。请奖项目：大气气溶胶化学、来源与演化机制。
与请奖项目有关的主要学术成就与创新点：①揭示了我国灰霾期间二次气溶胶对大气细颗粒物的重要贡献；②率先提出重霾期间二次有机气溶胶的贡献与二次无机气溶胶同等重要；③通过开展低温烟雾箱研究，揭示了低温、弱光照条件下二次有机气溶胶的快速生成机制；④较系统研究我国城市和高原地区大气气溶胶的理化特征、来源和时空分布特征。通过外场观测验证了海洋和极地大气边界层碘氧化物成核的大气新粒子生成机理新认识。
五篇代表性论著：
1.Huang RJ, Zhang YL, Bozzetti C, et al. 2014. High secondary aerosol contribution to particulate pollution during haze events in China. Nature, 514: 218-222.
2.Elser M, Huang RJ*, Wolf R, et al. 2016. New insights into PM2.5 chemical composition and sources in two major cities in China during extreme haze events using aerosol mass spectrometry. Atmos. Chem. Phys., 16: 3207-3225,.
3.Ho KF, Huang RJ, Kawamura K, et al. 2015. Dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls, fatty acids and benzoic acid in PM2.5 aerosol collected during CAREBeijing-2007: an effect of traffic restriction on air quality. Atmos. Chem. Phys., 15: 3111-3123.
4.Huang R J, Li WB, Wang YR, et al. 2014. Determination of aliphatic amines in atmospheric aerosol particles: A comparison of gas chromatography-mass spectrometry and ion chromatography approaches. Atmos. Meas. Tech., 7: 2027-2035.
5.Huang RJ, Seitz K, Neary T, O’Dowd CD, Platt U, Hoffmann T. 2010. Observations of high concentrations of I2 and IO in coastal air supporting iodine-oxide driven coastal new particle formation. Geophys. Res. Lett., 37: L03803, doi:10.1029/2009GL041467.
李 平，男，1981年8月生，中国科学院地球化学研究所研究员，博士。请奖项目：我国典型汞污染地区汞的环境污染和环境健康风险。
与请奖项目有关的主要学术成就与创新点：①证实食用大米可以是居民甲基汞暴露的主要途径，打破了“人类甲基汞暴露的主要途径是食用鱼和水产品”这一国际学术界传统认识，开创了人体甲基汞暴露全新的研究领域，建立了适用于食用大米人群甲基汞暴露的风险评估体系；②评估我国汞污染地区人群的无机汞暴露及健康风险；③开展我国典型汞污染地区的汞污染来源和环境过程研究，为汞污染地区的环境管理、环境污染治理和生态修复提供重要科学依据。
五篇代表性论著：
1.Li P, Du B, Maurice L, Laffont L, et al. 2017. Mercury isotope signatures of methylmercury in rice samples from the Wanshan mercury mining area, China: environmental implications. Environ. Sci. Technol., 51: 12321-12328.
2.Li P, Feng X, Chan HM, Zhang X, Du B. 2015. Human body burden and dietary methylmercury intake: the relationship in a rice-consuming population. Environ. Sci. Technol., 49: 9682-9689.
3.Li P, Feng X, Qiu G, Shang L, Wang S. 2012. Mercury pollution in Wuchuan mercury mining area, Guizhou, southwestern China: the impacts from large scale and artisanal mercury mining. Environment International, 42: 59-66.
4.Li P, Feng X, Yuan X, Chan HM, et al. 2012. Rice consumption contributes to low level methylmercury exposure in southern China. Environment International, 49:18-23.
5.Li P, Feng X, Qiu G, et al. 2009. Mercury pollution in Asia: a review of the contaminated sites. Journal of Hazardous Materials, 168: 591-601.
李高军，男，1983年8月生，南京大学教授，博士。请奖项目：地表过程同位素地球化学示踪。
与请奖项目有关的主要学术成就与创新点：①建立了钕、锶同位素亚洲风尘物源示踪体系，初步圈定了亚洲风尘物源区及其时空变化；②利用黄土证实了铀同位素破碎年代学理论；③开发了基于黄土生物微钙体元素组成的降水指标；④建立了基于海洋多同位素记录的碳循环逆向计算方法，证实玄武岩化学侵蚀受温度控制，从而提出基于玄武岩化学侵蚀反馈的碳循环平衡模型，为解决抬升驱动气候变化假说中碳循环不平衡问题提供了重要方案。
五篇代表性论著：
1.Li L, Liu XJ, Li T, Li LF, Zhao L, Ji JF, Chen J, Li GJ. 2017. Uranium comminution age tested by the eolian deposits on the Chinese Loess Plateau. Earth and Planetary Science Letters, 467: 64-71.
2.Li T, Liu F, Hemmo A Abels, You CF, Zhang ZK, Chen J, Ji JF, Li LF, Li L, Liu HC, Ren C, Xia RY, Zhao L, Zhang WF, Li GJ.2017. Continued obliquity pacing of East Asian summer precipitation after the mid-Pleistocene transition. Earth and Planetary Science Letters, 457: 181-190.
3.Li GJ, Hartmann Jens, Derry Louis A, et al. 2016. Temperature dependence of basalt weathering. Earth and Planetary Science Letters, 443: 59-69.
4.Li GJ, West Josh. 2014. Evolution of Cenozoic seawater lithium isotopes: Coupling of global denudation regime and shifting seawater sinks. Earth and Planetary Science Letters, 401: 284-293.
5.Li GJ, Elderfield Henry. 2013. Evolution of carbon cycle over the past 100 million years. Geochimica et Cosmochimica Acta, 103: 11-25.
李思亮，男，1978年10月，天津大学教授，博士。请奖项目：河流碳氮物质来源和关键过程辨识
与请奖项目有关的主要学术成就与创新点：①阐述西南喀斯特河流碳迁移以及其碳循环的复杂性，提出了C-S-N耦合对河流碳循环评估有重要影响的新认识，为准确评价区域或全球河流碳循环和动态变化格局提供了新的理论基础；②利用硝酸盐氮氧同位素解析了多个区域不同尺度河流硝氮来源，评估了反硝化过程对河流硝氮迁移转化的影响程度，揭示了气候因素和土地利用等对流域氮归趋的空间格局影响机制；③利用碳氮同位素和水化学对长江上游河流-水库体系物质迁移转化的研究，阐明了了水库大坝建设对河流-水库体系生物地球化学循环和碳氮物质的扰动机制。
五篇代表性论著：
1.Li SL, Calmels D, Han G, Gaillardet J, Liu CQ. 2008. Sulfuric acid as an agent of carbonate weathering constrained by d13CDIC: Examples from Southwest China. Earth and Planetary Science Letters, 170: 189-199.
2.Li SL, Liu CQ, Li J, et al. 2010. Assessment of the sources of nitrate in the Changjiang River, China using a nitrogen and oxygen isotopic approach. Environmental Science and Technology, 44: 1573-1578.
3.Li SL, Liu CQ, Li J, et al. 2010. Geochemistry of dissolved inorganic carbon and carbonate weathering in a small typical karstic catchment of Southwest China: Isotopic and chemical constraints. Chemical Geology, 277: 301-309.
4.Yue FJ, Li SL, Liu CQ, et al. 2015. Sources and transport of nitrate constrained by the isotopic technique in a karst catchment: an example from Southwest China. Hydrol. Process., 29: 1883-1893.
5.Zhong J, Li SL, Tao Fx, et al. 2017. Sensitivity of chemical weathering and dissolved carbon dynamics to hydrological conditions in a typical karst river. Scientific Reports: DOI: 10.1038/srep42944.
李雄耀，男，1978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：月壤特性与月球表面环境过程。
与请奖项目有关的主要学术成就与创新点：①解决尘埃静电迁移、太阳风注入和微陨石轰击过程模拟问题，建立了月球（行星）表面环境与资源利用研究平台，实现月面环境过程模拟和月壤特性分析的功能，填补国内实验条件空白，发展了月球与行星表面环境研究方向；②获取月面光照和水冰特性重要参数，揭示了月球南极永久阴影区中水冰的热行为特征以及中低纬度月球浅层基岩的埋藏特征；确定太阳风作用对矿物结构的损伤差异，提出微观结构指示太阳风暴露年龄的新思路；建立绝缘矿物功函数的测量方法，获取了月壤主要矿物的功函数，为载人空间应用发展战略和技术体系的制订及“空间环境模拟装置”大科学工程的实施提供参考；③突破亚微米级复杂形态颗粒破碎和纳米金属铁颗粒的溅射包裹技术，成功研制出平均粒径约400 nm具有纳米金属铁的CLDS-i高仿真模拟月尘；利用集宁玄武岩、磁铁矿和赤铁矿成功研制出JMSS/JMSD系列模拟火星样品，模拟样品被国内外科研院所广泛应用于工程测试和科学实验。
五篇代表性论著：
1.Gan H, Li XY, Wei Gf, Wang SJ. 2015. Work function measurements of olivine: Implication to photoemission charging properties in planetary environments. Advances in Space Research, 56(11): 2432-2438.
2.Zeng XJ, Li XY, Wang SJ, et al. 2015. JMSS-1: a new Martian soil simulant. Earth Planets and Space, 67: 1-10.
3.Li Y, Li XY, Wang SJ, et al. 2013. Crystal orientation results in different amorphization of olivine during solar wind implantation. Journal of Geophysical Research, 118(10): 1974-1982.
4.Tang H, Wang SJ, Li XY. 2012. Simulation of nanophase iron production in lunar space weathering. Planetary and Space Science, 60: 322-327.
5.Li XY, Wang SJ, Zheng YC, et al. 2008. Estimation of solar illumination on the Moon: A theoretical model. Planetary and Space Science, 56(7): 947-950.
梁晓亮，男，1984年1月生，中国科学院广州地球化学研究所副研究员，博士。请奖项目：类质同像置换对磁铁矿表面反应性的制约机制。
与请奖项目有关的主要学术成就与创新点：①率先开展天然磁铁矿的微结构与表面反应性研究，阐明天然磁铁矿的环境自净化能力及其制约因素，厘清磁铁矿在地球系统环境自净化过程中的作用与机制；②系统研究不同过渡金属类质同像置换对磁铁矿微结构与表面反应性的影响及其制约机制，揭示磁铁矿与典型环境物质的反应机理，为环境污染的治理与修复提供新思路；③创新性地将先进同步辐射技术及原位红外光谱技术引入磁铁矿微结构与表-界面反应机制研究，促进了矿物微结构与表面反应性研究的发展；④有效利用不同过渡金属对尖晶石结构进行精准调控，并通过多孔矿物负载减小尖晶石型复合氧化物的颗粒尺寸，研发高效的VOCs热催化氧化材料，拓宽了尖晶石型氧化物在大气污染治理中的应用前景。
五篇代表性论著：
1.Liang XL, Wei GL, Xiong J, et al. 2017. Adsorption isotherm, mechanism, and geometry of Pb(II) on magnetites substituted with transition metals. Chemical Geology, 470: 132-140.
2.Liang XL, Qi FH, Liu P, et al. 2016. Performance of Ti-pillared montmorillonite supported Fe catalysts for toluene oxidation: The effect of Fe on catalytic activity. Applied Clay Science, 132: 96-104.
3.Liang XL, He ZS, Tan W, et al. 2015. The oxidation state and microstructural environment of transition metals (V, Co, and Ni) in magnetite: an XAFS study. Physics and Chemistry of Minerals, 42(5): 373-383.
4.Liang XL, Li J, Joo JB, et al. 2012. Diffusion through the shells of yolk-shell and core-shell nanostructures in the liquid phase. Angewandte Chemie-International Edition, 51(32): 8034-8036.
5.Liang XL, Zhu SY, Zhong YH, et al. 2010. The remarkable effect of vanadium doping on the adsorption and catalytic activity of magnetite in the decolorization of methylene blue. Applied Catalysis B-Environmental, 97(1-2): 151-159.
刘超辉，男，1982年4月生，中国地质科学院地质研究所研究员，博士。请奖项目：华北克拉通元古宙构造盆地演化历史。
与请奖项目有关的主要学术成就与创新点：①准确厘定华北克拉通中部造山带周缘前陆盆地的形成时代和物源区性质；②准确限定赞皇杂岩中甘陶河群为2.1 Ga弧后盆地沉积产物；③率先提出吕梁杂岩存在古元古代中期俯冲大洋板片熔融作用的新认识；④首次根据北缘中-新元古代地层物源信息对罗迪尼亚超大陆复原图提供了新的约束。
五篇代表性论著：
1.Liu CH, Zhao GC, Sun M, et al. 2011. U-Pb and Hf isotopic study of detrital zircons from the Yejishan Group of the Lüliang Complex: Constraints on the timing of collision between the Eastern and Western Blocks, North China Craton. Sedimentary Geology, 236: 129-140.
2.Liu CH, Zhao GC, Sun M, et al. 2012. Detrital zircon U-Pb dating, Hf isotopes and whole-rock geochemistry from the Songshan Group in the Dengfeng Complex: Constraints on the tectonic evolution of the Trans-North China Orogen. Precambrian Research, 192-195: 1-15.
3.Liu CH, Zhao GC, Sun M, et al. 2012. U-Pb geochronology and Hf isotope geochemistry of detrital zircons from the Zhongtiao Complex: Constraints on the tectonic evolution of the Trans-North China Orogen. Precambrian Research, 222-223: 159-172.
4.Liu CH, Zhao GC, Liu FL, et al. 2012. Zircons U-Pb and Lu-Hf isotopic and whole-rock geochemical constraints on the Gantaohe Group in the Zanhuang Complex: Implications for the tectonic evolution of the Trans-North China Orogen. Lithos, 146-147: 80-92.
5.Liu CH, Zhao GC, Liu FL, Shi JR. 2014. Geochronological and geochemical constraints on the Lüliang Group in the Lüliang Complex: Implications for the tectonic evolution of the Trans-North China Orogen. Lithos, 198-199: 298-315.
彭君能，男，1981年3月生，中央研究院地球科学研究所助理研究员(台湾)，博士。请奖项目：伊朗–高加索碰撞造山带新生代岩浆活动之成因。
与请奖项目有关的主要学术成就与创新点：①通过对伊朗东部Lut-Sistan地区新生代岩浆岩的年代学、岩石学与地球化学研究，提出加厚地壳拆沉与软流圈地幔上涌的模型解释岩石成因，揭示该地区构造演化史复杂；②提出伊朗地区超钾质岩源自岩石圈地幔，由经过交代换质作用，含有金云母、石榴子石和磷灰石的地幔岩石部分熔融而成，微量元素比值显示交代换质作用有碳酸盐沉积物的参与；③对伊朗Anar地区一套埃达克质火山岩，通过年代学与地球化学实验，证明岩石成因不符合板片熔融假说，增厚地壳熔融更能说明火山岩喷发与阿拉伯–欧亚大陆碰撞的时空关系；④利用锆石铀-铅年代学与氩-氩年代学，提出伊朗Makran弧岩浆活动起始年龄为19 Ma之新观点。
五篇代表性论著：
1.Pang KN, Chung SL, Zarrinkoub MH, et al. 2016. New age and geochemical constraints on the origin of Quaternary adakite-like lavas in the Arabia-Eurasia collision zone. Lithos, 264: 348-359.
2.Pang KN, Chung SL, Zarrinkoub MH, et al. 2015. Quaternary high-Mg ultrapotassic rocks from the Qal’eh Hasan Ali maars, southeastern Iran: petrogenesis and geodynamic implications. Contributions to Mineralogy and Petrology, 170: 27.
3.Pang KN, Chung SL, Zarrinkoub MH, et al. 2014. On the magmatic record of the Makran arc, southeastern Iran: Insights from zircon U-Pb geochronology and bulk-rock geochemistry. Geochemistry, Geophysics, Geosystems, 15: 2151-2169.
4.Pang KN, Chung SL, Zarrinkoub MH, et al. 2013. Iranian ultrapotassic volcanism at ~11 Ma signifies the initiation of post-collisional magmatism in the Arabia-Eurasia collision zone. Terra Nova, 25: 405-413.
5.Pang KN, Chung SL, Zarrinkoub MH, et al. 2012. Age, geochemical characteristics and petrogenesis of Late Cenozoic intraplate alkali basalts in the Lut-Sistan region, eastern Iran. Chemical Geology, 306-307: 40-53.
谭静强，男，1983年1月生，中南大学教授，博士。请奖项目：南方海相页岩的生烃作用、富气机理和储层物性。
与请奖项目有关的主要学术成就与创新点：①揭示了我国南方下寒武统牛蹄塘组和下志留统龙马溪组海相页岩的初始有机质含量和初始生烃潜力，建立了生烃动力学模型，提出了生烃时限和生烃门限，论证了页岩油气在地质历史过程中的相态演变过程，为明确我国南方过成熟海相页岩的页岩气资源潜力提供了理论支撑；②深入研究了两套海相页岩对甲烷的吸附能力及主要控制因素，探讨了有机质、粘土矿物、孔隙结构、温度、压力等对页岩吸附能力的影响机制，为进一步探索页岩非均质性和储层地质条件对页岩含气性的影响奠定了科学基础；③率先研究并论证了两套海相页岩物质成分特征、岩石物理-力学性质和构造-沉积环境之间的耦合关系，揭示了低粘土矿物含量的海相页岩在不同种类、不同盐浓度的压裂液中浸泡后力学性质的变化规律，为深入探究页岩可压裂性、圈定页岩气勘探开发的有利区域提供了科学依据。
五篇代表性论著：
1.Tan JQ, Brian Horsfield, Nicolaj Mahlstedt, et al. 2013. Physical properties of petroleum formed during maturation of Lower Cambrian shale in the Upper Yangtze Platform, South China, as inferred from phase kinetics modelling. Marine and Petroleum Geology, 48: 47-56.
2.Tan JQ, Weniger Philipp, Bernhard Krooss, et al. 2014. Shale gas potential of the major marine shale formations in the Upper Yangtze Platform, South China, Part II: methane sorption capcity. Fuel, 129: 204-218.
3.Tan JQ, Brian Horsfield, Reinhard Fink, et al. 2014. Shale gas potential of the major marine shale formations in the Upper Yangtze Platform, South China, Part III: lithofacial, petrophysical, and rock mechanical properties. Energy & Fuels, 28: 2322-2342.
4.Tan JQ, Brian Horsfield, Nicolaj Mahlstedt, et al. 2015. Natural gas potential of Neoproterozoic and Lower Paleozoic marine shales in the Upper Yangtze Platform, South China: Geological and organic geochemical characterization. International Geology Review, 57: 305-326.
5.Qiao Lyu, Long XP, Ranjith PG, Tan JQ, et al. 2018. Experimental investigation on the mechanical behaviours of shale under water-based fluids. Engineering Geology, 233: 124-138.
王 伟，男，1984年7月生，中国地质大学（武汉）教授，博士。请奖项目：扬子陆块前寒武纪沉积盆地演化及超大陆重建。
与请奖项目有关的主要学术成就与创新点：①系统恢复扬子陆块早-中元古代沉积-岩浆-构造演化历程，证实扬子陆块与劳伦大陆西北缘的亲缘性，首次提出Columbia超大陆重建中的扬子-劳伦链接模式；②详细厘定扬子陆块东南缘新元古代沉积地质演化和盆山耦合过程，提供扬子陆块游离于罗迪尼亚超大陆外围的沉积学约束；③首次报道印度西北部新元古代低氧岩浆事件，提出Rodinia裂解过程中在超大陆边缘存在低氧岩浆带的模式，证实华南-印度在Rodinia超大陆中相连关系。
五篇代表性论著：
1.Wang W, Zhou MF, Yan DP, et al. 2012. Depositional age, provenance, andtectonic setting of the Neoproterozoic Sibao Group, southeastern Yangtze Block, South China. Precambrian Research, 192-195: 107-124.
2.Wang W, Peter Cawood, Zhou MF, Zhao JH. 2016. Paleoproterozoic magmatic and metamorphic events link Yangtze to northwest Laurentia in the Nuna supercontinent. Earth and Planetary Science Letters, 433: 269-279.
3.Wang W, Zhou MF. 2014. Provenance and tectonic setting of the Paleo- to Mesoproterozoic Dongchuan Group in the southwestern Yangtze Block, South China: implication for the breakup of the supercontinent Columbia. Tectonophysics, 610: 110-127.
4.Wang W, Zhou MF. 2013. Petrological and geochemical constraints on provenance, paleoweathering and tectonic setting of the Neoproterozoic sedimentary basin in the eastern Jiangnan Orogen, South China. Journal of Sedimentary Research, 83: 974-993
5.Wang W, Cawood PA, Zhou MF, et al. 2017. Low-δ18O rhyolites from the Malani Igneous Suite: a positive test for South China and NW India linkage in Rodinia. Geophysical Research Letters, 44: 10298-10305.
巫 翔，男，1978年9月生，中国地质大学（武汉）教授，博士。请奖项目：高压矿物物理。
与请奖项目有关的主要学术成就与创新点：①提出深俯冲带中铁自旋转变是下地幔中部地震波速不均一性机理之一；②率先开展了(Mg,Fe)SiO3后钙钛矿在核幔边界(D”层)温压条件下的变形原位测试实验，揭示了变形机制，并明确了环太平洋边界下D”层的剪切波速异常是由后钙钛矿择优排布所引起的；③查明高压下磷元素在铁磷合金中的赋存机制及状态，为讨论地核中轻元素的组成提供了依据。
五篇代表性论著：
1.Wu X, Lin JF, Kaercher P, et al.` 2017. Seismic anisotropy of the D” layer induced by (001) deformation of post-perovskite. Nature Communications, 8: 14669.
2.Wu X, Wu Y, Lin JF, et al. 2016. Two-stage spin transition of iron in FeAl-bearing phase D at lower mantle. Journal of Geophysical Research: Solid Earth, 121: 6411-6420.
3.Wu X, Mookherjee M, Gu TT, Qin S. 2011. Elasticity and anisotropy of iron-nickel phosphides at high pressures. Geophysical Research Letters, 38: L20301.
4.Wu X, Qin S, Gu TT, et al. 2011, Structural and elastic properties of CaGeO3 perovskite at high pressures. Physics of Earth and Planetary Interiors, 189: 151-156.
5.Wu X, Steinle-Neumann G, Narygina O, et al. 2009. High-pressure behavior of perovskite: FeTiO3 dissociation into (Fe1-δ,Tiδ)O and Fe1+δTi2-δO5. Physical Review Letters, 103: 065503.
夏琼霞，女，1979年2月生，中国科学技术大学特任副研究员，博士。请奖项目：大陆俯冲带超高压变质岩石学。
与请奖项目有关的主要学术成就与创新点：①准确识别出俯冲带变质岩石中多种成因的石榴石，阐释了变质过程中石榴石的多阶段生长特征；②有效识别出五种不同成因的变质锆石，建立了不同类型锆石的区分和识别依据，深化了变质锆石学，对解释锆石U-Pb定年及对应的地质事件具有重要指导意义；③率先在低温/超高压片麻岩中发现脱水熔融和超临界流体的岩石学和地球化学证据，提出大别超高压变质带经历热折返和部分熔融的新认识。
五篇代表性论著：
1.Xia QX, Wang HZ, Zhou LG, et al. 2016. Growth of metamorphic and peritectic garnets in ultrahigh-pressure metagranite during continental subduction and exhumation in the Dabie orogen. Lithos, 266-267: 158-181.
2.Xia QX, Zheng YF, Lu XN, et al. 2012. Formation of metamorphic and metamorphosed garnets in the low-T/UHP metagranite during continental collision in the Dabie orogen. Lithos, 136-139: 73-92.
3.Xia QX, Zheng YF, Hu ZC. 2010. Trace elements in zircon and coexisting minerals from low-T/UHP metagranite in the Dabie orogen: Implications for action of supercritical fluid during continental subduction-zone metamorphism. Lithos, 114: 385-412.
4.Xia QX, Zheng YF, Yuan HL, Wu FY. 2009. Contrasting Lu-Hf and U-Th-Pb isotope systematics between metamorphic growth and recrystallization of zircon from eclogite-facies metagranites in the Dabie orogen, China. Lithos, 112: 477-496.
5.Xia QX, Zheng YF, Zhou LG. 2008. Dehydration and melting during continental collision: Constraints from element and isotope geochemistry of low-T/UHP granitic gneiss in the Dabie orogen. Chemical Geology, 247: 36-65.
袁松虎，男，1979年6月生，中国地质大学（武汉）教授，博士。请奖项目：环境水文地球化学。
与请奖项目有关的主要学术成就与创新点：①揭示了地质过程中氧气进入地下水环境后会在二价铁矿物的作用下产生活性氧物质（如羟自由基），从而以地球化学机制氧化有害物质，为认识地下环境（有害）物质的有氧氧化提供了微生物之外的新机制；②阐明了硫铁矿活化氧气为活性氧物质的界面电子传递机制，揭示了二价铁粘土矿受氧气氧化时的电子由内向外的传递新过程；③提出了基于地下水电解产生氧气强化生成活性氧物质去除地下水中砷和氯代烃等有害物质的新方法。
五篇代表性论著：
1.Yuan SH, Liu XX, Liao WJ, et al. 2018. Mechanisms of electron transfer from structrual Fe(II) in reduced nontronite to oxygen for production of hydroxyl radicals. Geochimica et Cosmochimica Acta, 223: 422？436.
2.Zhang P, Yuan SH. Production of hydroxyl radicals from abiotic oxidation of pyrite by oxygen under circumneutral conditions in the presence of low-molecular-weight organic acids. Geochimica et Cosmochimica Acta, 218: 153-166.
3.Tong M, Yuan SH, Ma SC, et al. 2016. Production of abundant hydroxyl radicals from oxygenation of subsurface sediments. Environmental Science & Technology, 50: 214-221.
4.Yuan SH, Liao P, Alshawabkeh AN. Electrolytic manipulation of persulfate reactivity by iron electrodes for trichloroethylene degradation in groundwater. Environmental Science & Technology, 48: 656-663.
5.Yuan SH, Chen MJ, Mao XH, Alshawabkeh AN. 2013. Effects of reduced sulfur compounds on Pd-catalytic hydrodechlorination of TCE in groundwater using cathodic H2 under electrochemically-induced oxidizing conditions. Environmental Science & Technology, 47: 10502-10509.
赵晓丽，女，1981年6月生，中国环境科学研究院研究员，博士。请奖项目：纳米污染物环境地球化学行为研究。
与请奖项目有关的主要学术成就与创新点：①自主制备了一系列可用于对比研究、粒径/形貌均匀和表面结构可控的新型磁性纳米材料，率先开发了基于磁分离的环境水体痕量污染物快速分析新方法；②深入研究了Fe3O4 NPs等磁性纳米材料表面膜性质对PFCs、PAHs等典型污染物吸附作用机制，建立了表面活性剂类污染物在纳米材料表面自组装行为表征新方法，定量揭示了表面膜性质与污染物选择性作用机理；③综合对比研究了有机质、离子等水环境要素对Fe3O4 NPs环境行为复合影响作用机理，建立了河水、海水、湖水等自然水体中Fe3O4 NPs表面电势预测地球化学新模型,为纳米污染物环境行为与效应研究、风险评估和污染控制提供科学依据。
五篇代表性论著：
1.Zhao XL, Tang Z, Zhao TH. 2016. Magnetic nanoparticles interaction with humic acid: In the presence of surfactants. Environmental. Science & Technology, 50: 8640-8648.
2.Zhao XL, Hao W. 2015. Cetyltrimethylammonium bromide-coated Fe3O4 magnetic nanoparticles for analysis of 15 trace polycyclic aromatic hydrocarbons in aquatic environments by ultraperformance liquid chromatography with fluorescence detection. Analytical Chemistry, 87: 7667-7675.
3.Zhao XL, Liu SL. 2015. Surfactant-modified flowerlike layered double hydroxide-coatedmagnetic nanoparticles for preconcentration of phthalate esters from environmental water samples. Journal of Chromatography A, 1414: 22-30.
4.Zhao XL, Cai YQ, Wang T. 2008. Preparation of alkanethiolates functionalized core/shell Fe3O4@Au nanoparticles and its interaction with several typical target molecules. Analytical Chemistry, 80: 9091-9096.
5.Zhao XL, Shi YL, Cai YQ. 2008. Cetyltrimethylammonium bromide-coated magnetic nanoparticles for the preconcentration of phenolic compound from environmental water samples. Environmental Science & Technology, 42: 1201-1206.
赵新苗，女，1981年3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：华北岩石圈地幔Fe-Ca-Mg同位素地球化学特征。
与请奖项目有关的主要学术成就与创新点：①率先将新兴的Fe同位素示踪手段与传统的岩石地球化学方法相结合，开创性地研究了华北地区的地幔橄榄岩捕虏体，揭示了岩石圈地幔Fe同位素的高度不均一性；提出并论证了橄榄岩-熔体相互作用是岩石圈地幔Fe同位素组成不均一的重要机制，为橄榄岩-熔体反应在岩石圈地幔中的存在提供了明确的证据；②发现了迄今为止硅酸盐中最轻的Ca同位素组成，且和Fe同位素耦合，更新了长期以来人们对硅酸盐Ca同位素组成区间的认识；同时发现地幔中存在Ca、Fe同位素不平衡，论证了Ca、Fe同位素不平衡是地幔橄榄岩-熔体相互作用过程中元素扩散所引起的动力学分馏；揭示出造成地幔具有轻Ca、Fe同位素组成的熔体来源于软流圈；③首次对辉石岩捕掳体进行了Fe-Mg同位素组合研究，发现高压堆晶过程没有造成辉石岩明显的Fe-Mg同位素组成变化，而橄榄岩-熔体相互作用是导致辉石岩Fe-Mg同位素组成不均一的重要机制，为不同类型辉石岩的成因和来源提供了新的判别依据。
五篇代表性论著：
1.Zhao XM, Zhang ZF, Huang SC, et al. 2017. Coupled extremely light Ca and Fe isotopes in peridotites. Geochim. Cosmochim. Acta, 208: 368-380.
2.Zhao XM, Cao HH, Mi X, et al. 2017. Combined iron and magnesium isotope geochemistry of pyroxenite xenoliths from Hannuoba, North China Craton: implications for mantle metasomatism. Contrib. Mineral. Petrol, 172: 40-65.
3.Zhao XM, Zhang HF, Zhu XK, et al. 2015. Effects of melt percolation on iron isotopic variation in peridotites from Yangyuan, North China Craton. Chemical Geology, 401: 96-110.
4.Zhao XM, Zhang HF, Zhu XK, et al. 2012. Iron isotope evidence for multistage melt-peridotite interactions in the lithospheric mantle of eastern China. Chemical Geology, 292-293(23): 127-139.
5.Zhao XM, Zhang HF, Zhu XK, et al. 2010. Iron isotope variations in spinel peridotite xenoliths from North China Craton: implications for mantle metasomatism. Contrib. Mineral. Petrol., 160: 1-14.
左仁广，男，1981年11月生，中国地质大学（武汉）教授，博士。请奖项目：深层次矿化信息获取与集成。
与请奖项目有关的主要学术成就与创新点：①发现了岩浆热液矿床围绕控矿要素服从丛聚性分布的新规律，为解答矿床空间分布的争论提供了新证据；②揭示了勘查地球化学数据的闭合效应对地球化学异常识别的影响，研发了弱缓地球化学异常识别新技术，提高了弱缓地球化学异常识别能力；③揭示了不同误判代价对矿产预测结果的影响，提出了多源找矿信息融合新方法，提高了矿产预测的精度和效率。
五篇代表性论著：
1.Zuo R, Carranza EJM, Wang J. 2016. Spatial analysis and visualization of exploration geochemical data. Earth-Science Reviews, 158: 9-18.
2.Zuo R, Xiong Y. 2018. Big data analytics of identifying geochemical anomalies supported by machine learning methods. Natural Resources Research, 27: 5–13.
3.Zuo R, Zhang Z, Zhang D, et al. 2015. Evaluation of uncertainty in mineral prospectivity mapping due to missing evidence: a case study with skarn-type Fe deposits in Southwestern Fujian Province, China. Ore Geology Reviews, 71: 502–515.
4.Zuo R, Wang J. 2016. Fractal/multifractal modeling of geochemical data: A review. Journal of Geochemical Exploration, 164: 33–41.
5.Zuo R, 2014. Identification of geochemical anomalies associated with mineralization in the Fanshan district, Fujian, China. Journal of Geochemical Exploration, 139: 170–176.
所有获奖者符合本奖的奖掖条件，产生过程符合本奖《实施办法》所规定的程序。本奖的评选工作始终遵循办奖宗旨，遵循《实施办法》所规定的公平、公正和鼓励创新的原则。侯德封奖为发现人才、培养人才、推动学科发展发挥了重要作用，并得到了社会各界的广泛认同、赞赏与支持；我会将继续努力，为实现社会团体协助党和政府发展科学事业、促进出成果出人才，为建设创新型国家作出贡献。
上述21名获奖人，在矿物学、岩石学和地球化学研究领域做出了突出的创新性的贡献，是我国青年科学工作者的优秀代表；他们严谨求实、勇于探索创新的科学精神，他们报效祖国、服务社会的奉献精神，是值得提倡和学习的。
贵公网安备 52011502000706号 贵公网安备 52011502002779号
