【文章內(nèi)容簡(jiǎn)介】 ou, ., Zhu, B., Liu, F., Gong, ., Huang, ., Xiao, Y., Chen, C., He, ., 2015. Iron and magnesium isotope fractionation in oceanic lithosphere and subarc mantle: perspectives from ophiolites. Earth and Planetary Science Letters 430, 523532.3. Su, ., Qin, ., Tang, ., Sakyi, ., Liu, ., Sun, H., Xiao, ., 2013. Late Paleozoic maficultramafic intrusions in southern Central Asian Orogenic Belt (NW China): insight into magmatic NiCu sulfide mineralization in orogenic setting. Ore Geology Reviews 51, 5773.4. Su, ., Qin, ., Sakyi, ., Li, ., Yang, ., Sun, H., Tang, ., Liu, ., Xiao, ., Malaviarachchi, ., 2011. UPb ages and HfO isotopes of zircons from Late Paleozoic maficultramafic units in southern Central Asian Orogenic Belt: tectonic implications and evidence for an EarlyPermian mantle plume. Gondwana Research 20, 516531.5. Su, ., Zhang, ., Sakyi, ., Yang, ., Ying, ., Tang, ., Qin, ., Xiao, Y., Zhao, ., Mao, Q., Ma, ., 2011. The origin of spongy texture of mantle xenolith minerals from the Western Qinling, Central China. Contributions to Mineralogy and Petrology 161, 465482.汪福順，男，1976年4月生，上海大學(xué)教授，博士。請(qǐng)獎(jiǎng)項(xiàng)目：河流攔截蓄水的環(huán)境影響。與請(qǐng)獎(jiǎng)項(xiàng)目有關(guān)的主要學(xué)術(shù)成就及創(chuàng)新點(diǎn)：①更新了國(guó)際上對(duì)水庫(kù)溫室氣體釋放的認(rèn)識(shí)；提出了高壩大庫(kù)溫室氣體釋放的研究方法和評(píng)估要點(diǎn)；建立了一套適合水庫(kù)溫室氣體大面觀測(cè)的走航式連續(xù)觀測(cè)系統(tǒng)。首次對(duì)我國(guó)全流域梯級(jí)開(kāi)發(fā)的河流進(jìn)行了梯級(jí)水庫(kù)二氧化碳釋放進(jìn)行了全面評(píng)估，做出了不支持國(guó)際上在熱帶地區(qū)水庫(kù)進(jìn)行的結(jié)論；提出了我國(guó)亞熱帶水庫(kù)的溫室氣體釋放特點(diǎn)，并建立了水庫(kù)溫室氣體釋放的滯留時(shí)間模式。②研究了大規(guī)模梯級(jí)筑壩對(duì)河流中以硅為主線的營(yíng)養(yǎng)鹽的攔截效應(yīng)。③首次估算了長(zhǎng)江流域水面的CO2釋放通量，提出了自然水體也是大氣溫室氣體重要來(lái)源的觀點(diǎn)。④用碳、氮穩(wěn)定同位素及放射性同位素定年技術(shù)，揭示了滇池水體富營(yíng)養(yǎng)化演變的發(fā)生、發(fā)展過(guò)程，反演了污染物入湖歷史及主要來(lái)源；發(fā)展了氮穩(wěn)定同位素技術(shù)在研究水體富營(yíng)養(yǎng)化中的應(yīng)用。五篇代表性論著：1. Fushun Wang*, Man Cao, Baoli Wang, et al., Seasonal variation of CO2 diffusion flux from a large subtropical reservoir in East China. Atmospheric Environment. 2015,103: 129137.2. Guo, JH. Wang, FS. Vogt,RD et al. Anthropogenically enhanced chemical weathering and carbon evasion in the Yangtze Basin. Scientific Reports. 5, 11941。 doi: (2015). 3. Fushun Wang, et al. Carbon dioxide emission from surface water in cascade reservoir river system on the Maotiao River, southwest of China. Atmospheric Environment. 2011, 45: 38273834. 4. Fushun Wang, et al. Dissolved silicate retention and transport in cascade reservoirs in Karst area, Southwest China. Science of total environment. 2010, 408(7):16671675. 5. FuShun Wang, et al. Stable Isotopes in Sedimentary Organic Matter from Lake Dianchi and their Indication of Eutrophication History. Water Air Soil Pollut. 2009,199: 159170. 王孝磊，男，1979年6月生，南京大學(xué)教授，博士。請(qǐng)獎(jiǎng)項(xiàng)目：華南前寒武紀(jì)構(gòu)造巖漿演化和花崗巖成因。與請(qǐng)獎(jiǎng)項(xiàng)目有關(guān)的主要學(xué)術(shù)成就與創(chuàng)新點(diǎn)：①理清了江南造山帶的構(gòu)造巖漿演化過(guò)程，明確其在全球新元古代構(gòu)造演化中的意義。系統(tǒng)厘定了江南造山帶內(nèi)不整合面之下“褶皺基底”地層的時(shí)代，論證了江南造山帶從“碰撞后”到“造山后”不同階段巖漿作用的表現(xiàn)，所提出的江南造山帶構(gòu)造巖漿演化模式較好地解釋了揚(yáng)子地塊東南緣新元古代巖漿作用的地球動(dòng)力學(xué)過(guò)程。②通過(guò)礦物微區(qū)原位分析技術(shù)，識(shí)別出源區(qū)過(guò)程和熔融機(jī)制對(duì)于花崗巖形成的制約因素，提供了花崗巖漿熔體成分變化的HfO同位素證據(jù)，對(duì)過(guò)渡型花崗巖的成因給出了合理的解釋?zhuān)皇状卧趪?guó)際上提出源區(qū)“鋯石效應(yīng)”和地殼的不平衡熔融可能是造成花崗巖鋯石Hf同位素變化的主要原因；對(duì)放射性損傷在鋯石原位元素和同位素分析上進(jìn)行了全面的評(píng)估。五篇代表性論著：1. Wang XL*, Zhou JC, Wan YS, Kitajima K, Wang D, Bonamici C, Qiu JS, Sun T, Magmatic evolution and crustal recycling for Neoproterozoic strongly peraluminous granitoids from southern China: Hf and O isotopes in zircon. Earth and Planetary Science Letters 366, 71–82 (2013).2. Wang XL*, Zhou JC, Griffin WL, Zhao GC, Yu JH, Qiu JS, Zhang YJ, Xing GF, Understanding the contrasting geochemical features of the crust in the Jiangnan Orogen. Precambrian Research 242, 154171 (2014).3. Wang XL*, Coble MA, Valley JW, Shu XJ, Kitajima K., Spicuzza ., Sun T., Influence of radiation damage on Late Jurassic zircons from southern China: evidence from in situ measurements of oxygen isotopes, laser Raman, UPb ages, and trace elements. Chemical Geology 389, 122136, (2014).4. Tang M, Wang XL*, Shu XJ, Yang T, Wang D, Gopon P, Hafnium isotopic heterogeneity in zircons from granitic rocks: geochemical evaluation and modeling of zircon effect in crustal anatexis. Earth and Planetary Science Letters 389, 188199 (2014).5. Xing GF*, Wang XL*, Wan YS, Chen ZH, Jiang Y, Kitajima K, Ushikubo T, Gopon P, Diversity in early crustal evolution: 4100 Ma zircons in the Cathaysia Block of southern China. Scientific Reports 4, 5143, (2014). 吳懷春，男，1977年12月生，中國(guó)地質(zhì)大學(xué)（北京）教授，博士。請(qǐng)獎(jiǎng)項(xiàng)目：米蘭科維奇沉積旋回與高精度天文地質(zhì)年代。與請(qǐng)獎(jiǎng)項(xiàng)目有關(guān)的主要學(xué)術(shù)成就與創(chuàng)新點(diǎn)：①確定出地球軌道參數(shù)深刻地影響著二疊紀(jì)氣候和沉積過(guò)程；建立了中二疊世羅德階–三疊紀(jì)印度階天文年代標(biāo)尺, 完成中二疊世早三疊世牙形石帶、生物大滅絕和重大地質(zhì)事件年齡及持續(xù)時(shí)間的高精度年代標(biāo)定, 確定出煤山剖面二疊紀(jì)末期生物大滅絕事件持續(xù)時(shí)間為~, 穩(wěn)定碳同位素急劇負(fù)偏持續(xù)時(shí)間為~ 萬(wàn)年。②在松遼盆地及遼西的陸相白堊系識(shí)別出完整的米蘭科維奇沉積旋回, 證明了地球軌道力深刻地影響著溫室條件下陸地環(huán)境的氣候變化和沉積過(guò)程。 建立了“松科1井”持續(xù)時(shí)間長(zhǎng)達(dá)28 Ma的長(zhǎng)偏心率天文年代標(biāo)尺, 完善了松遼盆地上白堊統(tǒng)高精度年代格架及其與海相地層的對(duì)比方案。③建立了中國(guó)南海北部中新世以來(lái)完整的地磁極性年代格架。五篇代表性論著：1. Wu Huaichun, Zhang Shihong, Hinnov Linda, Jiang Ganqing, Yang Tianshui, Li Haiyan, Wan Xiaoqiao, Wang Chengshan. Cyclostratigraphy and orbital tuning of the terrestrial upper SantonianLower Danian in Songliao Basin, northeastern China. Earth and Planetary Science Letters, 2014, 407: 8295. 2. Wu Huaichun, Zhao Xixi, Shi Meinan, Zhang Shihong, Li Haiyan, Yang Tianshui. A 23 Myr magnetostratigraphic time framework for Site 1148, ODP Leg 184 in South China Sea and its geological implications. Marine and Petroleum Geology, 2014, 58: 749759. 3. Wu Huaichun, Zhang Shihong, Hinnov Linda, Feng Qinglai, Jiang Ganqing, Li Haiyan, Yang Tianshui. Timecalibrated Milankovitch cycles for the late Permian. Nature Communications, 2013, 4: 2452. doi: 4. Wu Huaichun