Mantle-like to low oxygen isotopes in zircon from the mid-Cretaceous high-silica granites reveal unweathered basement recycling along the present coastal area of SE China

Zircon oxygen isotope compositions can provide potential constraints on the origin of granitic magmas. In this work, we report new data of zircon U-Pb dating, trace elements and Hf-O isotopes for two types of mid -Cretaceous high-silica granites from Zhoushan archipelago in Zhejiang Province, SE China. The in-situ zircon data are carefully screened for radiation damage and post-magmatic alteration. The analyzed magmatic zircon grains indicate that the Zhoushan calc-alkaline granites (ZCAG; 101-92 Ma) have mantle-like 818O values of 5.29-5.88 %o, in contrast to the Zhoushan peralkaline granites (ZPAG; 91-89 Ma) with relatively low 818O of 4.42-4.6 %o. The slight decreases in 818O and epsilon Hf(t) from zircon center to periphery of both groups suggest that they may have consistent oxygen isotopic compositions in their parental magma sources and have gone through assimilations to hydrothermally altered wall rocks in the shallow crust. The mantle-like 818O values in zircon are widespread in the Cretaceous felsic rocks in the present coastal area of SE China, which, in combination Hf isotopes, indicates the possible existence of a buried unweathered Proterozoic basement in the eastern part of the Cathaysia Block. This work highlights the role of deep crustal magma sources, assimilation and post-magmatic radioactive damage on the formation of mantle-like to low 818O signals in zircons, and has fundamental im-plications for understanding the formation of widespread mid-Cretaceous felsic rocks along the present coastal area of SE China.