- 姓名: 吴超
- 性别: 男
- 职务:
- 职称: 副研究员
- 学历: 博士研究生
- 电话:
- 传真:
- 电子邮件: wuchao@gig.ac.cn
- 通讯地址: 广州市天河区科华街511号
主要从事斑岩型铜-金-钼矿床成矿机制与勘查研究工作,包括成矿模型和大区域控矿因素分析研究。主持或参与国家自然科学青年基金、科技部重点研发项目、中科院战略先导专项、科技部973等项目的研究。目前以第一作者/通讯作者发表SCI论文10篇。受邀在2019年第九届全国成矿理论与找矿方法学术研讨会和2020年第十五届全国矿床会议作主题报告。
教育经历
2013/09-2018/06,中国科学院大学,矿物学、岩石学、矿床学,博士研究生(直博)
2017/03-2018/03,澳大利亚塔斯马尼亚大学国家矿产研究中心,矿床学,联合培养博士研究生
2009/09-2013/06,中国地质大学(武汉),资源勘查工程(工科基地班),学士
工作经历
2022/12-至今,中国科学院广州地球化学研究所,副研究员
2018/07-2022/12,中国科学院广州地球化学研究所,博士后
简 历:
社会任职:
斑岩铜矿多尺度成矿规律与勘查应用
研究方向:
广州地化所博士后学术年会报告一等奖(2021),二等奖(2020)
“涂光炽优秀青年学者计划”A类(2023)
获奖及荣誉:
[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] 陈华勇*,吴超,2020,俯冲带斑岩铜矿系统成矿机理与主要挑战 中国科学:地球科学,v. 50,p. 865-886.
[17] 梁培,陈华勇*,韩金生,吴超,张维峰,赵联党,王云峰,2017,东准噶尔北缘早石炭世构造体制转变:来自碱性花岗岩年代学和地球化学制约. 大地构造与成矿学,v. 41,p. 202-221.
代表论著:
国家自然科学基金青年基金项目:哈腊苏斑岩铜矿带岩浆温度、氧逸度和H2O-F-Cl-SO3等挥发分含量对成矿的指示:来自矿物化学成分的制约,2020/01-2022/12,27万元,主持