Faculty Profile
  ZHAO Zifu
Department: School of Earth and Space Science
Mailing Address:
School of Earth and Space Science, University of Science and Technology of China, 96 Jinzhai Rd, Hefei, Anhui, 230026, PR China
Postal Code:

Research Profile

      under construction ......
Selected Publications
1) Origin of syn-collisional granitoids in the Gangdese orogen: Reworking of the juvenile arc crust and the ancient continental crust , Geological Society of America Bulletin , 2021 ,
2) 1. Zircon U-Pb ages, Hf and O isotopes constrain the crustal architecture of the ultrahigh-pressure Dabie orogen in China. (SCI) , Chemical Geology , 200805 ,
3) Magma differentiation and recharge in the petrogenesis of early paleozoic mafic intrusives in the Qilian orogen, northwestern China , Lithos , 2021 ,
4) 2. Element mobility in mafic and felsic ultrahigh-pressure metamorphic rocks during continental collision. (SCI) , Geochimica et Cosmochimica Acta , 200711 ,
5) Syn-exhumation melting of the subducted continental crust: Geochemical evidence from early Paleozoic granitoids in North Qaidam, northern Tibet , Lithos , 2020 ,
6) 3. Comment on “Paleozoic ages and excess 40Ar in garnets from the Bixiling eclogite in Dabieshan, China: New insights from 40Ar/39Ar dating by stepwise crushing” by Qiu and Wijbrans (2006). (SCI) , Geochimica et Cosmochimica Acta , 200712 ,
7) Geochemical evidence for the production of granitoids through reworking of the juvenile mafic arc crust in the Gangdese orogen, southern Tibet , Geological Society of America Bulletin , 2020 ,
8) 4. Mineral oxygen isotope and hydroxyl content changes in ultrahigh-pressure eclogite-gneiss contacts from Chinese Continental Scientific Drilling Project cores. (SCI) , Journal of Metamorphic Geology , 200702 ,
9) Syn-exhumation magmatism during continental collision: Geochemical evidence from the early Paleozoic Fushui mafic rocks in the Qinling orogen, Central China , Lithos , 2020 ,
10) Post-collisional granitoids from the Dabie orogen in China: Zircon U-Pb age, element and O isotope evidence for recycling of subducted continental crust. (SCI) , Lithos , 200702 ,
11) Whole-rock geochemical and zircon Hf–O isotopic constraints on the origin of granitoids and their mafic enclaves from the Triassic Mishuling pluton in West Qinling, central China , Journal of Asian Earth Sciences , 2020 ,
12) 6. Diffusion compensation for argon, hydrogen, lead, and strontium in minerals: Empirical relationships to crystal chemistry. (SCI) , American Mineralogist , 200702 ,
13) The geochemical nature of mantle sources for two types of Cretaceous basaltic rocks from Luxi and Jiaodong in east-central China , Lithos , 2019 ,
14) 7. Isotopic constraints on age and duration of fluid-assisted high- pressure eclogite-facies recrystallization during exhumation of deeply subducted continental crust in the Sulu orogen. (SCI) , Journal of Metamorphic Geology , 200610 ,
15) 8. Zircon U-Pb age, element and C-O isotope geochemistry of post- collisional mafic-ultramafic rocks from the Dabie orogen in east-central China. (SCI) , Lithos , 200507 ,
16) 9. Zircon isotope evidence for recycling of subducted continental crust in post- collisional granitoids from the Dabie terrane in China. (SCI) , Geophysical Research Letters , 200411 ,
17) Temporal relationship between granite cooling and hydrothermal uranium mineralization at Dalongshan in China: a combined radiometric and oxygen isotopic study. (SCI) , Ore Geology Reviews, , 200410 ,
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