Mo-rich source and protracted crystallization of Late Mesozoic granites in the East Qinling porphyry Mo belt (central China): Constraints from zircon U/Pb ages and Hf-0 isotopes

摘要

In the East Qinling orogenic belt, central China, there are numerous Mo deposits with over 6 Mt Mo metal. The giant Nannihu, Shangfanggou and Yuchiling porphyry Mo deposits are hosted in porphyry stocks associated with the Heyu batholith, whereas the giant Donggou porphyry Mo deposit is hosted in a stock associated with the Taishanmiao batholith. Zircon grains from the Heyu batholith have concordant U-238/Pb-206 ages scattered from 150 +/- 3 to 130 +/- 2 Ma with an age interval of nearly 20 my., whereas ore-hosting granitic porphyry stocks from the Nannihu, Shangfanggou and Yuchiling deposits have Pb-206/U-238 ages ranging from 151 +/- 1 to 135 +/- 1 Ma, 143 +/- 1 to 132 +/- 1 Ma, and 143 +/- 5 to 131 +/- 5 Ma, respectively. It is likely that the Heyu batholith has a prolonged history of incremental assembly and the ore-bearing granitic porphyry stocks may have originated from the same magma reservoir and emplaced in different stages. Likewise, zircon grains from the Taishanmiao batholith have concordant U-238/Pb-206 ages spanning in a period from 130 +/- 2 to 111 +/- 3 Ma, whereas those from the Donggou granitic porphyry stock have U-238/Pb-206 ages ranging from 125 +/- 2 to 110 +/- 3 Ma, nearly coeval with the Taishanmiao batholith. The molybdenite Re-Os model ages for each deposit are coincident with relatively young zircon U-238/Pb-206 ages of the host stock, indicating that Mo mineralization is likely related to late-stage magmatism. Zircon grains from the batholiths and granitic porphyry stocks have epsilon(H)(f)(t) ranging from -10 to - 30, T-DM(2) ages from 1.6 to 2.5 Ga and delta O-18 from +5.0 to +8.7%s, which are taken to suggest the involvement of the subducted continental crust of the Yangtze Block in the source. We thus propose that the extensive Mo mineralization in the East Qinling porphyry Mo belt is genetically related to the prolonged granitic magmatism in the Late Mesozoic and a Mo-rich source that was related to the subducted continental crust of the Yangtze Block stagnating beneath the southern margin of the North China Craton.