李歡[中南大學地質資源系特聘教授]

李歡，男，漢族，中南大學地質資源系特聘教授，1985年10月生，湖南省瀏陽市人。2008年、2011年分別獲中南大學工學學士（地質工程礦產勘查方向）、碩士（礦產普查與勘探）學位；2011年被錄取為國家公派研究生赴日本九州大學攻讀博士學位，2014年畢業後作為海外優秀博士人才引進回國，入職中國地質大學（武漢），並於2016年遴選為首批“地大學者”，2018年起任中南大學地球科學與信息物理學院教授。工學博士，研究生導師，研究方向：構造與成礦、岩石礦床大地構造、成礦規律與成礦預測。日本資源地質學會會員，國際SCI刊物《Ore Geology Reviews》、《International Geology Review》、《Journal of Asian Earth Sciences》、《Canadian Journal of Earth Sciences》、《Chemie der Erde - Geochemistry》、《Earth Sciences Research Journal》及《Journal of Earth Science》審稿人。截至2018年3月，以第一作者且通訊作者身份發表國際SCI論文15篇（總影響因子>40）、EI論文2篇，論文被引100餘次。曾赴日本、捷克、德國、美國、英國、新加坡、蒙古國、印度、印度尼西亞、中國等國參加國際會議十餘次並作口頭報告，發表國際會議論文十餘篇，主要會議為：日本(CINEST Symposium 2011、Asia-Africa Mineral Resources Conference 2011、日本資源地質學會第63回年會學術講演會)、印度（G-COE 9th Symposium）、新加坡(GEOS 2012)、印度尼西亞 (Asia-Africa Mineral Resources Conference 2012)、蒙古國(Asia-Africa Mineral Resources Conference 2013)、德國(GeoMod2014)、英國(VMSG 2014)、美國(Goldschimidt 2014)、香港(PACRIM2015) 、捷克 (Goldschimidt 2015)。主持包括國家自然科學基金在內的科研項目6項，作為骨幹人員參與國際合作項目、國家重點研究計畫、國家自然科學基金面上項目及國家省部級項目和橫向課題20餘項，野外研究主要集中在湖南錫礦山銻礦，河南省陝縣大方山、葫蘆峪金礦，湖南平江蛇行山鉛鋅礦，青海省大柴旦紅燈溝金礦，青海省茫崖虎頭崖多金屬礦，廣西平果鋁土礦，印度尼西亞萬丹省Neglasari金礦，青海省玉樹趙卡隆鐵銅多金屬礦，郴州坪寶地區寶山鉛鋅礦、香花嶺錫鉛鋅礦、黃沙坪鉛鋅礦、大坊金礦、柿竹園多金屬礦床，內蒙古太僕寺旗金豆子山金礦，河北張家口東坪金礦，湖南板溪銻礦，印度尼西亞Krakatau活火山，日本鹿兒島縣菱刈（Hishikari）金礦，蒙古國Borro金礦和Erdent斑岩銅礦，英國Arthor’s Seat 火山，美國加利福尼亞－內華達州金礦，印度那格譜爾多金屬礦，膠東三山島北部海域、蠶莊及九曲金礦等。科研合作夥伴主要有日本Koichiro Watanabe 教授、Kotaro Yonezu副教授以及Thomas Tindell助理教授，克羅地亞Ladislav antun palinkaš教授，澳大利亞Noreen Evans教授、Martin Danisik高級研究員，美國Thomas Algeo教授，菲律賓Jillian Aira S. Gabo-Ratio助理教授等。 現指導研究生5人，其中國外留學生2人。

結合國際前沿熱點，廣泛開展國際合作，在構造與成礦領域開展了深入研究。1）提出了海底噴流礦床“沉積扇”新構造成因模式。該模式系統總結了不同構造環境中的海底噴流礦床的特徵及控制機理，確定了海底噴流礦床最終定位及礦床特徵空間變異的構造控制機制，指出中繼斜坡構造控制了成礦流體遷移、定位及礦體的空間分布。該構造模式被成功運用到錫鐵山、趙卡隆、虎頭崖等礦床深部礦體的預測中。2）發現了不同構造－岩漿環境下熱液礦物形成機理的差異，厘定了構造驅動熱液流體的性質及其源區特徵。總結了湘南多金屬礦集區不同成礦構造中熱液礦物的產出形式，揭示了湘南多期次成礦流體構造－岩漿屬性。3）建立了華南南嶺侏羅紀大地構造－岩漿－成礦的多階段複雜過程模型，探索性地進行了華南侏羅紀岩石圈伸展演化規律的總結，闡述了岩石圈不同的伸展速率對成礦岩體的上升及冷卻速率的控制，指出不同大地構造形式控制了岩體的上升及冷卻速率，進而對多金屬礦化過程起到至關重要作用。4）基於華北北緣新發現的W-Mo-Pb-Zn多金屬礦床進行了大地構造的成因模式研究，建立了三疊世－侏羅世礦床演化序列及與對應大地構造背景的關聯，認為在古亞洲洋的俯衝背景下，大地構造的演化控制了高－中－低溫礦床組合。基於礦床大地構造的成因模式，圈定了找礦靶區，取得了較好的經濟效益。5）探索了成礦後構造過程對礦床的影響，運用低溫熱年代學對膠東相關金礦進行了隆升剝露差異的構造改造對比研究，指出焦家式金礦成礦後剝露程度應強於玲瓏式金礦，玲瓏式金礦下部有存在焦家式金礦的可能。

代表性論文

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A newly found biotite syenogranite in the Huangshaping polymetallic deposit, South China: Insights into Cu mineralization. Journal of Earth Science, doi: 10.1007/s12583-017-0974-7 (IF=0.975, JCR四區). 5. Wu, J.H., Li, H*., Xi, X.S., Kong, H., Wu, Q.H., Peng, N.L., Wu, X.M., Cao, J.Y., Gabo-Ratio, J.A.S., 2017. Geochemistry and geochronology of the mafic dikes in the Taipusi area, northern margin of North China Craton: Implications for Silurian tectonic evolution of the Central Asian Orogen. Journal of Earth System Science 126:64, DOI: 10.1007/s12040-017-0841-z. (IF=0.955, JCR四區) 6. Sun, H.S., Li, H*., Evans, N.J., Yang, H., Wu, P., 2017c. Volcanism, mineralization and metamorphism at the Xitieshan Pb–Zn deposit, NW China: Insights from zircon geochronology and geochemistry. Ore Geology Reviews 88, 289–303. (IF=3.095, JCR一區) 7. Li, H*., Yonezu, K., Watanabe, K., Tindell, T., 2017b. Fluid origin and migration of the Huangshaping W–Mo polymetallic deposit, South China: Geochemistry and 40Ar/39Ar geochronology of hydrothermal K-feldspars. Ore Geology Reviews 86, 117–129. (IF=3.095, JCR一區) 8. Li, H., Sun, H.S*., Wu, J.H., Evans, N.J., Xi, X.S., Peng, N.L., Cao, J.Y., Gabo-Ratio, J.A.S., 2017a. Re–Os and U–Pb geochronology of the Shazigou Mo polymetallic ore field, Inner Mongolia: Implications for Permian–Triassic mineralization at the northern margin of the North China Craton, Ore Geology Reviews 83, 287–299. (IF=3.095, JCR一區) 9. Sun, H.S., Li, H*., Danišík, M., Xia, Q.L., Jiang, C.L., Wu, P., Yang, H., Fan, Q.R., Zhu, D.S., 2017b. U–Pb and Re–Os geochronology and geochemistry of the Donggebi Mo deposit, Eastern Tianshan, NW China: Insights into mineralization and tectonic setting. Ore Geology Reviews 86, 584–599. (IF=3.095, JCR一區) 10. Sun, H.S., Li, H*., Liu, L., Chen, Q.M., Yang, H., Wu, P., 2017a. 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