赵子福
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·Paper Publications
- [1] Dai, F.-Q., *Zhao, Z.-F., Zheng, Y.-F., Sun, G.-C., 2019. The geochemical nature of mantle sources for two types of Cretaceous basaltic rocks from Luxi and Jiaodong in east-central China. Lithos 344-345, 409-424..
- [2] *Zhao, Z.-F., Zheng, Y.-F., Chen, Y.-X., Sun, G.-C., 2017. Partial melting of subducted continental crust: Geochemical evidence from synexhumation granite in the Sulu orogen. Geological Society of America Bulletin 129, 1692-1707..
- [3] *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..
- [4] Dai, F.-Q., *Zhao, Z.-F., Zheng, Y.-F., 2017. Partial melting of the orogenic lower crust: Geochemical insights from post-collisional alkaline volcanics in the Dabie orogen. Chemical Geology 454, 25-43..
- [5] Lu, Y.-H., *Zhao, Z.-F., Zheng, Y.-F., 2017. Geochemical constraints on the nature of magma sources for Triassic granitoids from South Qinling in central China. Lithos 284-285, 30-49..
- [6] Dai, F.-Q., *Zhao, Z.-F., Dai, L.-Q., Zheng, Y.-F., 2016. Slab–mantle interaction in the petrogenesis of andesitic magmas: Geochemical evidence from postcollisional intermediate volcanic rocks in the Dabie orogen, China. Journal of Petrology 57(6), 1109-1134..
- [7] Lu, Y.-H., *Zhao, Z.-F., Zheng, Y.-F., 2016. Geochemical constraints on the source nature and melting conditions of Triassic granites from South Qinling in central China. Lithos 264, 141-157..
- [8] *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..
- [9] *Zhao ZF, Dai LQ, Zheng YF. 2015. Two types of the crust-mantle interaction in continental subduction zones. Science China: Earth Sciences 58 (8), 1269-1283..
- [10] *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..