赵新福 (教授)

教授 博士生导师 硕士生导师

曾获荣誉:2016年中国地质大学十大杰出青年

性别:男

毕业院校:香港大学

学历:研究生(博士)毕业

学位:博士

在职信息:在职

所在单位:资源学院

职务:资源系系主任

学科:矿产普查与勘探 矿物学、岩石学、矿床学

办公地点:主楼721室

Email:

个人简历

一、个人简介 

男,1982年生,江苏镇江人。 

2004年6月毕业于中国地质大学(武汉)资源勘查工程基地班,获学士学位;2006年6月获得中国地质大学(武汉) 矿物学、岩石学、矿床学硕士学位,2010年1月获得香港大学矿床学博士学位。2010-2013年在香港大学从事博士后研究工作。2013年4月回母校中国地质大学(武汉)资源学院工作。主要从事热液矿床的成矿作用机理研究,主要研究方向为岩浆热液铁-铜-金-稀土成矿系统。主持和参与了多项国家自然科学基金和科技部重点研发项目,发表SCI论文50余篇,包括第一作者或通讯作者在Economic Geology,Mineralium Deposita,Geochimica et Cosmochimica Acta,Chemical Geology和American Mineralogist等矿床学和矿床地球化学的重要期刊上发表论文约20篇,论文SCI引用超2000次。 

Researchgate: Researchgate主页

Google scholar: scholar主页


二、教学情况 

本科生课程:《矿床地球化学》、《矿床学》

研究生课程:《高级矿床学》、《矿床学理论与矿产勘查前沿》、《区域成矿学》


三、主要研究方向和研究兴趣 

1、岩浆热液铁-铜-金-稀土成矿系统:包括铁氧化物-铜-金(IOCG)矿床、玢岩铁矿(IOA)、矽卡岩型矿床和碳酸岩相关的稀土矿床等

2、盆地流体铜-铅-锌-铀成矿系统

3、成因矿物学反演热液成矿系统形成和演化过程及其找矿指示 

4、华南前寒武纪构造演化与成矿作用


四、近期主要研究项目 

[1] 蚀变矿物和流体包裹体卤族元素LA-ICPMS原位分析对热液矿床成因的指示: 以长江中下游成矿带为例 (国家自然科学基金面上项目,编号41972074 ,2020-2023),主持

[2] 矿床学(国家自然科学基金优秀青年项目,编号41822203,2019-2021),主持

[3] 华北克拉通破坏成矿响应的集成研究(国家自然科学重大研究计划集成项目,编号91514303,2016-2017),主持

[4] 康滇铁铜成矿带典型矿床成矿机制:矿物微区地球化学和年代学制约(国家自然科学面上项目,编号41472068,2014-2018),主持

[5] 华北东部巨量金来源、迁移与富集机理(国家重点研发计划深地资源勘查开采专项,编号2016YFC0600104,2016-2020),参加

[6] 稀有金属元素成矿的构造-岩浆深部过程(科技部深地资源探测专项项目,编号2017YFC0602401,2017-2021),参加

[7] 矽卡岩型富铁矿形成机制及控制因素(国家重点基础研究发展计划(973计划)课题,编号2012CB416802: 2012-2016),参加


五、代表性论文

29) Xiong, L., Zhao, X.*, Wei, J., Jin, X., Fu, L., Lin, Z., 2020. Linking Mesozoic lode gold deposits to metal-fertilized lower continental crust in the North China Craton: Evidence from Pb isotope systematics. Chemical Geology: 119440.

28) Zhao, X.-F., Chen, W.-T., Li, X.-C., Zhou, M.-F.*, 2019. Iron Oxide Copper-Gold Deposits in China: A Review and Perspectives on Ore Genesis. In: Goldfarb, R., Chang, Z. (Eds.), Mineral Deposits of China. SEG Special Publication. Volume 22, 553-580.

27) Su, Z.-K., Zhao, X.-F.*, Zeng, L.-P., Zhao, K.-D., Hofstra, A.H., 2019. Tourmaline boron and strontium isotope systematics reveal magmatic fluid pulses and external fluid influx in a giant iron oxide-apatite (IOA) deposit. Geochimica et Cosmochimica Acta, 259: 233-252.

26) Zeng, L.-P., Zhao, X.-F.*, Hammerli, J., Fan, T.-W.-T., Spandler, C., 2019. Tracking fluid sources for skarn formation using scapolite geochemistry: an example from the Jinshandian iron skarn deposit, Eastern China. Mineralium Deposita. DOI:10.1007/s00126-019-00914-3

25) Su, J.-H., Zhao, X.-F.*, Li, X.-C., Hu, W., Chen, M., Xiong, Y.-L., 2019. Geological and geochemical characteristics of the Miaoya syenite-carbonatite complex, Central China: Implications for the origin of REE-Nb-enriched carbonatite. Ore Geology Reviews, 113: 103101.

24) 赵新福*, 李占轲*, 赵少瑞, 毕诗健, 李建威, 2019. 华北克拉通南缘早白垩世区域大规模岩浆-热液成矿系统. 地球科学, 44(1): 52-68.

23) 李建威, 赵新福, 邓晓东, 谭俊, 胡浩, 张东阳, 李占轲, 李欢, 荣辉, 杨梅珍, 曹康, 靳晓野, 隋吉祥, 俎波, 昌佳, 吴亚飞, 文广, 赵少瑞 2019. 新中国成立以来中国矿床学研究若干重要进展. 中国科学:地球科学, 49: 1720-1771.

22) 林祖苇, 赵新福*, 熊乐, 朱照先, 2019. 胶东三山岛金矿床黄铁矿原位微区微量元素特征及对矿床成因的指示. 地球科学进展, 34(4): 399-413.

21) 陈伟, 赵新福, 李晓春, 周美夫, 2019. 中国铁氧化物-铜-金(IOCG)矿床的基本特征及研究进展. 岩石学报, 35(1): 99-118.

20) 纪敏, 赵新福*, 曾丽平, 范田纬腾, 2018. 鄂东南铜绿山矿床石榴子石显微结构及微区成分对成矿过程的指示. 岩石学报, 34(9): 2716-2732.

19) Zhao, X.-F.*, Zhou, M.-F., Su, Z.-K., Li, X.-C., Chen, W.T., Li, J.-W., 2017. Geology, geochronology, and geochemistry of the Dahongshan Fe-Cu-(Au-Ag) deposit, SW China: Implications for the formation of IOCG deposits in intracratonic rift settings. Economic Geology, 112(3): 603-628.

18) Zhao, X.-F.*, Su, Z.-K., Zeng, L.-P., 2017. Genetic models of IOCG and IOA deposits from China: Implications for ore genesis and their possible links, Proceedings of the 14th SGA Biennial Meeting. IOCG-IOA ore systems and their magmatic-hydrothermal continuum: A family reunion?, Québec City, pp. 835-838.

17) Bi, S.-J., Zhao, X.-F.*, 2017. 40Ar/39Ar dating of the Jiehe gold deposit in the Jiaodong Peninsula, eastern North China Craton: Implications for regional gold metallogeny. Ore Geology Reviews, 86: 639-651.

16) Zeng, L.-P., Zhao, X.-F. *, Li, X.-C., Hu, H., McFarlane, C., 2016. In situ elemental and isotopic analysis of fluorapatite from the Taocun magnetite-apatite deposit, Eastern China: Constraints on fluid metasomatism. American Mineralogist, 101(11): 2468-2483.

15) Su, Z.-K., Zhao, X.-F. *, Li, X.-C., Zhou, M.-F., 2016. Using elemental and boron isotopic compositions of tourmaline to trace fluid evolutions of IOCG systems: The worldclass Dahongshan Fe-Cu deposit in SW China. Chemical Geology, 441: 265-279.

14) Zhao, X.-F. *, Zhou, M.-F., Gao, J.-F., Li, X.-C., Li, J.-W., 2015. In situ Sr isotope analysis of apatite by LA-MC-ICPMS: constraints on the evolution of ore fluids of the Yinachang Fe-Cu-REE deposit, Southwest China. Mineralium Deposita, 50(7): 871-884.

13) Li, X., Zhao, X., Zhou, M.-F., Chen, W.T., Chu, Z., 2015. Fluid inclusion and isotopic constraints on the origin of the Paleoproterozoic Yinachang Fe-Cu-(REE) deposit, southwest China. Economic Geology, 110(5): 1339-1369.

12) Zhou, M.-F., Zhao, X.-F., Chen, W.T., Li, X.-C., Wang, W., Yan, D.-P., Qiu, H.-N., 2014. Proterozoic Fe-Cu metallogeny and supercontinental cycles of the southwestern Yangtze Block, southern China and northern Vietnam. Earth-Science Reviews, 139(0): 59-82.

11) Zhao, X.-F., Zhou, M.-F., Li, J.-W., Selby D., Li C., Li X.-H. and Qi, L., 2013. Sulfide Re–Os and Rb–Sr isotopic ages and the tectonic environment of the Kangdian Fe–Cu metallogenic province, SW China. Economic Geology, 108(6): 1489-1498.

10) Zhao, X.-F., Zhou, M.-F., Li, J.-W., and Qi, L., 2013. Late Paleoproterozoic sediment-hosted stratiform copper deposits in South China: Their possible link to the supercontinent cycle. Mineralium Deposita, 48(1): 129-136.

9) Huang, X.-W., Zhao, X.-F.*, Qi, L., Zhou, M.-F., 2013. Re-Os and S isotopic constraints on the origins of two mineralization events at the Tangdan sedimentary rock-hosted stratiform Cu deposit, SW China. Chemical Geology, 347(0): 9-19.

8) Zhao, X.-F., Zhou, M.-F., Hitzman, M.W., Li, J.-W., Bennett, M., Meighan, C. and Anderson, E., 2012. Late Paleoproterozoic to Early Mesoproterozoic Tangdan Sedimentary Rock-Hosted Strata-bound Copper Deposit, Yunnan Province, Southwest China. Economic Geology, 107: 357-375.

7) Zhao, X.-F. and Zhou, M.-F., 2011. Fe–Cu deposits in the Kangdian region, SW China: A Proterozoic IOCG (iron-oxide–copper–gold) metallogenic province. Mineralium Deposita 46: 731-747.

6) Zhao, X.-F., Zhou, M.-F., Li, J.-W., Sun, M., Gao, J.-F., Sun, W.-H., Yang, J.-H., 2010. Late Paleoproterozoic to early Mesoproterozoic Dongchuan Group in Yunnan, SW China: Implications for tectonic evolution of the Yangtze Block. Precambrian Research, 182: 57-69.

5) Li, J.-W., Zhao, X.-F., Zhou, M.-F., Ma, C.-Q., de Souza, Z. and Vasconcelos, P., 2009. Late Mesozoic magmatism from the Daye region, eastern China: U–Pb ages, petrogenesis, and geodynamic implications. Contributions to Mineralogy and Petrology, 157: 383-409.

4) Li, J.-W., Zhao, X.-F., Zhou, M.-F., Vasconcelos, P., Ma, C.-Q., Deng, X.-D., de Souza, Z.S., Zhao, Y.-X., Wu, G., 2008. Origin of the Tongshankou porphyry–skarn Cu–Mo deposit, eastern Yangtze craton, Eastern China: geochronological, geochemical, and Sr–Nd–Hf isotopic constraints. Mineralium Deposita, 43(3): 315-336. 

3) Zhao, X.-F., Zhou, M.-F., Li, J.-W., and Wu, F.-Y., 2008. Association of Neoproterozoic A- and I-type granites in South China: Implications for generation of A-type granites in a subduction-related environment. Chemical Geology, 257:1-15.

2) 赵新福, 李建威, 马昌前, 郎银生, 2007. 北淮阳古碑花岗闪长岩侵位时代及地球化学特征: 对大别山中生代构造体制转换的启示. 岩石学报,  23(6): 1392-1402.

1) 赵新福, 李建威, 马昌前, 2006. 鄂东南铁铜矿集区铜山口铜(钼)矿床40Ar /39Ar年代学及对区域成矿作用的指示. 地质学报, 80(6): 849-862.



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