办公电话：

邮箱： zfzhao@ustc.edu.cn

科研领域： 主要从事大陆俯冲带岩浆岩成因、超高压变质岩化学地球动力学、稳定同位素分馏系数和元素扩散系数计算及其地球化学应用等方面的研究。




个人简介
1973年1月出生于四川省南部县。教授，博士生导师。1996年获中国科学技术大学理学学士学位(地球化学)，2001年获中国科学技术大学理学博士学位(地球化学)。2001年8月至今在中国科学技术大学从事教学和科研工作，2004年1月被聘为副教授，2008年1月被聘为教授。获2004年国家自然科学奖二等奖(排名第二)，2005年入选教育部“新世纪优秀人才支持计划”，获2006年“侯德封奖”、2009年“孙贤鉥奖”、2015年教育部自然科学一等奖(第三完成人)。2011年获得“国家****科学基金”。


课题&项目
1. 国家****科学基金
2. 国家973项目课题
3. 中国科学院先导专项子课题
4. 国家重点研发计划专题
5. 国家自然科学基金面上项目


发表文章
Dai,F.-Q., *Zhao, Z.-F., Zheng, Y.-F., Sun, G.-C., 2019. The geochemical nature ofmantle sources for two types of Cretaceous basaltic rocks from Luxi andJiaodong in east-central China. Lithos 344-345, 409-424.
*Zhao,Z.-F., Zheng, Y.-F., Chen, Y.-X., Sun, G.-C., 2017. Partial melting ofsubducted continental crust: Geochemical evidence from synexhumation granite inthe Sulu orogen. Geological Society of America Bulletin 129, 1692-1707.
*Zhao,Z.-F., Liu, Z.-B., Chen, Q., 2017. Melting of subducted continental crust:Geochemical evidence from Mesozoic granitoids in the Dabie-Sulu orogenic belt,east-central China. Journal of Asian Earth Sciences 145, 260-277.
Dai,F.-Q., *Zhao, Z.-F., Zheng, Y.-F., 2017. Partial melting of the orogenic lowercrust: Geochemical insights from post-collisional alkaline volcanics in theDabie orogen. Chemical Geology 454, 25-43.
Lu,Y.-H., *Zhao, Z.-F., Zheng, Y.-F., 2017. Geochemical constraints on the natureof magma sources for Triassic granitoids from South Qinling in central China.Lithos 284-285, 30-49.
Dai,F.-Q., *Zhao, Z.-F., Dai, L.-Q., Zheng, Y.-F., 2016. Slab–mantle interaction inthe petrogenesis of andesitic magmas: Geochemical evidence from postcollisionalintermediate volcanic rocks in the Dabie orogen, China. Journal of Petrology57(6), 1109-1134.
Lu,Y.-H., *Zhao, Z.-F., Zheng, Y.-F., 2016. Geochemical constraints on the sourcenature and melting conditions of Triassic granites from South Qinling incentral China. Lithos 264, 141-157.
*Zhao, Z.-F., Gao, P., Zheng, Y.-F., 2015. The source of Mesozoic granitoids in South China: Integrated geochemical constraints from the Taoshan batholith in the Nanling Range. Chemical Geology 395, 11-26.
*ZhaoZF, Dai LQ, Zheng YF. 2015. Two types of the crust-mantle interaction incontinental subduction zones. Science China: Earth Sciences 58 (8), 1269-1283.
*Zhao, Z.-F., Dai, L.-Q., Zheng, Y.-F. 2013. Postcollisional mafic igneous rocks record crust-mantle interaction during continental deep subduction. Scientific Reports 3, 3413; DOI:10.1038/srep03413.
Zhang, J., *Zhao, Z.-F., Zheng, Y.-F., Liu, X.M., Xie, L.W., 2012. Zircon Hf-O isotope and whole-rock geochemical constraints on origin of postcollisional mafic to felsic dykes in the Sulu orogen. Lithos, 136-139, 225-245.
Yang, Q.-L., *Zhao, Z.-F., Zheng, Y.-F., 2012. Modification of subcontinental lithospheric mantle above continental subduction zone: Constraints from geochemistry of Mesozoic gabbroic rocks in southeastern North China. Lithos 146-147, 164-182.
Xu, Z., *Zhao, Z.-F., Zheng, Y.-F., 2012. Slab-mantle interaction for thinning of cratonic lithospheric mantle in North China: Geochemical evidence from Cenozoic continental basalts in central Shandong. Lithos 146-147, 202-217.
*Zhao, Z.-F., Zheng, Y.-F., Zhang, J., Dai, L.-Q., Li, Q., Liu, X., 2012. Syn-exhumation magmatism during continental collision: Evidence from alkaline intrusives of Triassic age in the Sulu orogen. Chemical Geology 328, 70-88.
Dai, L.-Q., *Zhao, Z.-F., Zheng, Y.-F., Zhang, J., 2012. The nature of orogenic lithospheric mantle: Geochemical constraints from postcollisional mafic-ultramafic rocks in the Dabie orogen. Chemical Geology 334, 99-121.
Yang, Q.-L., *Zhao, Z.-F., Zheng, Y.-F., 2012. Slab-mantle interaction in continental subduction channel: Geochemical evidence from Mesozoic gabbroic intrusives in southeastern North China. Lithos 155, 442-460.
Dai, L.-Q., *Zhao, Z.-F., Zheng, Y.-F., Li, Q.L., Yang, Y.H., Dai, M.N., 2011. Zircon Hf-O isotope evidence for crust-mantle interaction during continental deep subduction. Earth and Planetary Science Letters, 308 (1-2), 229-244.
*Zhao, Z.-F., Zheng, Y.-F., Wei, C.-S., Wu, F.-Y., 2011. Origin of postcollisional magmatic rocks in the Dabie orogen: Implications for crust-mantle interaction and crustal architecture. Lithos, 126 (1-2), 99-114.
Wang, Y., *Zhao, Z.-F., Zheng, Y.-F., Zhang, J.-J., 2011. Geochemical constraints on the nature of mantle source for Cenozoic continental basalts in east-central China. Lithos, 125 (3-4), 940-955.
Zhang,J., *Zhao, Z.-F., Zheng, Y.-F., Dai, M., 2010. Postcollisional magmatism: Geochemical constraints onthe petrogenesis of Mesozoic granitoids in the Sulu orogen, China. Lithos 119,512-536.
*ZhaoZF,Zheng YF., 2009. Remelting of subducted continental lithosphere: Petrogenesisof Mesozoic magmatic rcoks in the Dabie-Sulu orogenic belt. Science in China(Series D-Earth Sciences),52(9), 1295-1318.
*Zhao,Z.-F., Zheng, Y.-F., Wei ,C.-S., Chen, F.-K., Liu, X., Wu, F.-Y.,2008. Zircon U-Pb ages, Hf and O isotopes constrain the crustalarchitecture of the ultrahigh-pressure Dabie orogen in China. Chemical Geology253, 222-242.
*Zhao Z.-F., Gao T.-S., 2007. Comment on “Paleozoic ages and excess ⁴⁰Arin garnets from the Bixiling eclogite inDabieshan,China: Newinsights from ⁴⁰Ar/³⁹Ar dating by stepwise crushing” byQiu and Wijbrans (2006). Geochimica et Cosmochimica Acta 71(24), 6046-6050.
*Zhao, Z.-F., Zheng, Y.-F.,Chen, R.-X., Xia, Q.-X., Wu, Y.-B., 2007. Element mobility in mafic and felsicultrahigh-pressure metamorphic rocks during continental collision. Geochimica et CosmochimicaActa 71, 5244-5266.
*Zhao, Z.-F., Chen, B., Zheng,Y.-F., Chen, R.-X., Wu, Y.-B., 2007. Mineral oxygen isotope and hydroxyl contentchanges in ultrahigh-pressure eclogite–gneiss contacts from Chinese ContinentalScientific Drilling Project cores. Journal of Metamorphic Geology 25, 165-186.
Zhao, Z.-F. *Zheng, Y.-F.,2007. Diffusioncompensation for argon, hydrogen, lead, and strontium in minerals: Empiricalrelationships to crystal chemistry. American Mineralogist 92, 289-308.
*Zhao, Z.-F., Zheng, Y.-F.,Wei, C.-S., Wu, Y.-B., 2007. Post-collisional granitoids from the Dabie orogen inChina: Zircon U–Pb age, element and Oisotope evidence for recycling of subducted continental crust. Lithos 93,248-272.
*Zhao, Z.-F., Zheng, Y.-F., Gao, T.-S., Wu, Y.-B., Chen,B., Chen, F.-K.,Wu, F.-Y., 2006. Isotopicconstraints on age and duration of fluid-assisted high-pressure eclogite-faciesrecrystallization during exhumation of deeply subducted continental crust inthe Sulu orogen. Journal of Metamorphic Geology 24, 687-702.
*Zhao,Z.-F., Zheng, Y.-F., Wei, C.-S., Wu, Y.-B., Chen, F.K.,Jahn, B.-m., 2005. ZirconU-Pb age, element and C-O isotope geochemistry of post-collisionalmafic-ultramafic rocks from the Dabie orogen in east-centralChina. Lithos83, 1-28.
*Zhao, Z.–F., Zheng, Y.–F., Wei,C.-S.,Wu, Y.–B., 2004. Zircon isotope evidence for recycling of subductedcontinental crust in post-collisional granitoids from the Dabie terrane in China.Geophysical Research Letters VOL. 31, L22602, doi:10.1029/2004GL021061.
Zhao, Z.–F., *Zheng, Y.–F., Wei,C.-S.,Gong, B., 2004. Temporal relationship betweengranite cooling and hydrothermal uranium mineralization at Dalongshan in China: a combined radiometric and oxygen isotopicstudy. Ore Geology Reviews 25, 221-236.
Zhao. Z.-F.,*Zheng, Y.-F., 2003. Calculation of oxygenisotope fractionation in magmatic rocks. Chemical Geology193, 59-80.
Zhao,Z.-F., *Zheng, Y.-F., Wei, C.-S., Gong B., 2001. Carbonconcentration and isotope composition of granites from southeastern China. Physicsand Chemistry of Earth 26, 821-833.