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教授
- 电子邮箱：3a7ff718c4d25deadbe64c22126216e8dd6a54c8441c3d4f3879bbec6a91b8c0371cf762b9dffe5d41e22f76f7e127f86eddee9af0a0e8a09c142a37b0a8808abb3d663759fe14392b8ef6d9a6d399d5de07d16250d94f5c3c2e1b18c0763358b7cb0e1d8764768b5da2fa329901bf34df45fb47199b78e450a33438a3ec9a0d
- 联系方式：0551-63600093
- 学位：博士
访问量：
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[31]Zhao, Z.–F., *Zheng, Y.–F., Wei, C.-S., Gong, B., 2004. Temporal relationship between granite cooling and hydrothermal uranium mineralization at Dalongshan in China: a combined radiometric and oxygen isotopic study. Ore Geology Reviews 25, 221-236..
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[32]Zhao. Z.-F., *Zheng, Y.-F., 2003. Calculation of oxygen isotope fractionation in magmatic rocks. Chemical Geology 193, 59-80..
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[33]Zhao, Z.-F., *Zheng, Y.-F., Wei, C.-S., Gong B., 2001. Carbon concentration and isotope composition of granites from southeastern China. Physics and Chemistry of Earth 26, 821-833.
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[34]赵子福,赵子福.Postcollisional mafic igneous rocks record crust-mantle interaction
during continental deep subduction.SCIENTIFIC REPORTS,2013,3
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[35]赵子福,赵子福.Partial melting of subducted continental crust: Geochemical evidence
from synexhumation granite in the Sulu orogen.GEOLOGICAL SOCIETY OF AMERICA BULLETIN,129(11-12):1692-1707.
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[36]赵子福,赵子福.Melting of subducted continental crust: Geochemical evidence from
Mesozoic granitoids in the Dabie-Sulu orogenic belt, east-central China.JOURNAL OF ASIAN EARTH SCIENCES,2017,145260-277.
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[37]赵子福,赵子福.The source of Mesozoic granitoids in South China: Integrated geochemical
constraints from the Taoshan batholith in the Nanling Range.CHEMICAL GEOLOGY,2015,39511-26.
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[38]赵子福,赵子福.Two types of the crust-mantle interaction in continental subduction
zones.SCIENCE CHINA-EARTH SCIENCES,2015,58(8):1269-1283.
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[39]赵子福.Slab-mantle interaction in continental subduction channel: Geochemical
evidence from Mesozoic gabbroic intrusives in southeastern North China.LITHOS,2012,155442-460.
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[40]赵子福.Geochemical constraints on the nature of magma sources for Triassic
granitoids from South Qinling in central China.LITHOS,2017,28430-49.
