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              • 姓名： 吳超
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              • 性別： 男
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              • 職務(wù)： 
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              • 職稱(chēng)： 副研究員
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              • 學(xué)歷： 博士研究生
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              • 電話(huà)： 
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              • 傳真： 
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              • 電子郵件： wuchao@gig.ac.cn
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              • 通訊地址： 廣州市天河區科華街511號
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                簡(jiǎn)　　歷：
                
                                
              • 　　主要從事斑巖型銅-金-鉬礦床成礦機制與勘查研究工作，包括成礦模型和大區域控礦因素分析研究。主持或參與國家自然科學(xué)青年基金、科技部重點(diǎn)研發(fā)項目、中科院戰略先導專(zhuān)項、科技部973等項目的研究。目前以第一作者/通訊作者發(fā)表SCI論文10篇。受邀在2019年第九屆全國成礦理論與找礦方法學(xué)術(shù)研討會(huì )和2020年第十五屆全國礦床會(huì )議作主題報告。
                 

                　　教育經(jīng)歷
                 

                　　2013/09-2018/06，中國科學(xué)院大學(xué)，礦物學(xué)、巖石學(xué)、礦床學(xué)，博士研究生（直博）
                 

                　　2017/03-2018/03，澳大利亞塔斯馬尼亞大學(xué)國家礦產(chǎn)研究中心，礦床學(xué)，聯(lián)合培養博士研究生
                 

                　　2009/09-2013/06，中國地質(zhì)大學(xué)（武漢），資源勘查工程（工科基地班），學(xué)士
                 

                　　工作經(jīng)歷
                 

                　　2022/12-至今，中國科學(xué)院廣州地球化學(xué)研究所，副研究員
                 

                　　2018/07-2022/12，中國科學(xué)院廣州地球化學(xué)研究所，博士后
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                社會(huì )任職：
                
                                
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                研究方向：
                
                                
              • 　　斑巖銅礦多尺度成礦規律與勘查應用
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                獲獎及榮譽(yù)：
                
                                
              • 　　廣州地化所博士后學(xué)術(shù)年會(huì )報告一等獎（2021），二等獎（2020）
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                代表論著(zhù)：
                
                                
              • [1] Wu, C., Chen, H., Chiaradia, M., Huangfu, P., and Li, Z., 2024, Linking Pacific Plate formation and Early Cretaceous metallogenic response on the circum-Pacific continental margins: GSA Bulletin, v. 136, p. 171-183.
   
                 

                [2] Wu, C., Chiaradia, M., Tang, G., and Chen, H., 2023, Crustal control on the petrogenesis of adakite-like rocks: Chemical Geology, v. 632, p. 121548.
                 

                [3] Wu, C., Chen, H.*, and Lu, Y.*, 2022, Crustal structure control on porphyry copper systems in accretionary orogens: insights from Nd isotopic mapping in the Central Asian Orogenic Belt: Mineralium Deposita, v. 57, p. 631-641.
                 

                [4] Duan, G., Wu, C.*, Baker, M.J., Qi, J., Xu, C., and Zhang, L., 2022, Evolution and genesis of hydrothermal fluids for the Cretaceous Dongnan Cu deposit, Zijinshan ore district (SE China): Ore Geology Reviews, v. 144, p. 104844.
    
                 

                [5] Sun, W., Feng, Y., Zhu, Z., Zhang, S., Jiang, H., and Wu, C.*, 2022, Episodic ore-forming fluid evolution processes in the Jiudian gold deposit, Jiaodong Peninsula: Constrains from texture, trace element and S isotope composition of pyrite: Ore Geology Reviews, v. 148, p. 105023.
    
                 

                [6] Wu, C., Chen, H.*, and Lu, Y.*, 2021, Magmatic Water Content and Crustal Evolution Control on Porphyry Systems: Insights from the Central Asian Orogenic Belt: Journal of Petrology, v. 62, p. 1-15.
    
                 

                [7] Chen, H.*, and Wu, C., 2020, Metallogenesis and major challenges of porphyry copper systems above subduction zones: Science China Earth Sciences, v. 63, p. 899-918.
    
                 

                [8] Liang, P.*, Wu, C.*, Hu, X., and Xie, Y., 2020, Textures and geochemistry of magnetite: Indications for genesis of the Late Paleozoic Laoshankou Fe-Cu-Au deposit, NW China: Ore Geology Reviews, v. 124, p. 103632.
    
                 

                [9] Liang, P., Chen, H.*, Han, J., Wu, C., Zhang, W., Xu, D., Lai, C., and Kyser, K., 2019, Iron oxide-copper-gold mineralization of the Devonian Laoshankou deposit (Xinjiang, NW China) in the Central Asian Orogenic Belt: Ore Geology Reviews, v. 104, p. 628-655.
    
                 

                [10] Wu, C., Chen, H.*, Hong, W., Li, D., Liang, P., Fang, J., Zhang, L., and Lai, C., 2019, Magnetite chemistry and implications for the magmatic-hydrothermal ore-forming process: An example from the Devonian Yuleken porphyry Cu system, NW China: Chemical Geology, v. 522, p. 1-15.
    
                 

                [11] Feng, Y., Xiao, B.*, Li, R., Deng, C., Han, J., Wu, C., Li, G., Shi, H., and Lai, C., 2019, Alteration mapping with short wavelength infrared (SWIR) spectroscopy on Xiaokelehe porphyry Cu-Mo deposit in the Great Xing’an Range, NE China: Metallogenic and exploration implications: Ore Geology Reviews, v. 112, p. 103062.
    
                 

                [12] Wu, C., Chen, H.*, Liang, P., Han, J.S., Liu, Z.J., Fang, J., and Xu, D.R., 2018, Paragenesis and fluid evolution of the Halasu III porphyry Cu deposit, East Junggar (NW China): Implications for the Paleozoic multiphase superimposing mineralization in the Central Asian Orogenic Belt: Ore Geology Reviews, v. 100, p. 183-204.
    
                 

                [13] Liang, P., Chen, H.*, Wu, C., Zhang, W.F., Xu, D.R., Xia, X.P., Liu, Z.J., and Zhang, Z.J., 2017, Mineralization and ore genesis of the Qiaoxiahala Fe-Cu-(Au) deposit in the northern margin of East Junggar terrane, Central Asian Orogenic Belt: Constraints from fluid inclusions and stable isotopes: Ore Geology Reviews, v. 100, p. 360-384.
    
                 

                [14] Xu, C., Chen, H.*, Qi, J., Duan, G., Zhang, L., Wu, C., Zhang, S., and Zhong, W., 2016, Mesozoic multiphase magmatism at the Xinan Cu–Mo ore deposit (Zijinshan Orefield): Geodynamic setting and metallogenic implications: Ore Geology Reviews, v. 88, p. 768-790.
    
                 

                [15] Liang, P., Chen, H.*, Hollings, P., Wu, C., Xiao, B., Bao, Z., and Xu, D., 2016, Geochronology and Geochemistry of Igneous Rocks from the Laoshankou District, North Xinjiang: Implications for the Late Paleozoic Tectonic Evolution and Metallogenesis of East Junggar: Lithos, v. 266-267, p. 115-132.
    
                 

                [16] 陳華勇*，吳超，2020，俯沖帶斑巖銅礦系統成礦機理與主要挑戰 中國科學(xué):地球科學(xué)，v. 50，p. 865-886. 
    
                 

                [17] 梁培，陳華勇*，韓金生，吳超，張維峰，趙聯(lián)黨，王云峰，2017，東準噶爾北緣早石炭世構造體制轉變：來(lái)自堿性花崗巖年代學(xué)和地球化學(xué)制約. 大地構造與成礦學(xué)，v. 41，p. 202-221.
   
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                承擔科研項目情況：
                
                                
              • 　　國家自然科學(xué)基金青年基金項目：哈臘蘇斑巖銅礦帶巖漿溫度、氧逸度和H2O-F-Cl-SO3等揮發(fā)分含量對成礦的指示：來(lái)自礦物化學(xué)成分的制約，2020/01-2022/12，27萬(wàn)元，主持
                 

                 
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