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    Timing of skarn deposit formation of the Tonglushan ore district, southeastern Hubei Province, Middle–Lower Yangtze River Valley metallogenic belt and its implications [查看] GuiqingXie、JingwenMao、HaijieZhao、KetaoWei、ShangguangJin、HuijunPan、YufuKe
    The Tonglushan ore district in theMiddle–Lower Yangtze River Valleymetallogenic belt includes the Tonglushan Cu–Fe, the Jiguanzui Au–Cu, and the Taohuazui Au–Cu skarn deposits. They are characterized by NE-striking ore bodies and hosted at the contact of Triassic carbonate rocks and Late Mesozoic granitoid deposits. New Sensitive High-Resolution Ion Microprobe (SHRIMP) and Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA–ICP-MS) zircon U–Pb,molybdenite Re–Os, and phlogopite 40Ar–39Ar ages indicate that these skarn deposits formed between 140.3±1.1 and 137.3±2.4 Ma. These dates are identical to the zircon U–Pb ages for host quartz diorites ranging from 140±2 to 139±1 Ma. These results confirm that both skarn mineralization and related intrusions were initiated during the Early Cretaceous. The high rhenium contents (261.4–1152 μg/g) of molybdenites indicate that ametasomaticmantle fluidwas involved in the ore-forming process of these skarn ore systems. This conclusion is consistent with previously published constraints from sulfur, deuterium, and oxygen isotope compositions, and the geochemical signatures, and Sr–Nd isotopic data of the mineralization-hosting intrusions. Geological and geochronological evidence demonstrates that there were two igneous events in the Tonglushan ore district. The first resulted in the emplacement of quartz diorite during the Early Cretaceous (140±2 to 139±1 Ma), and the second is characterized by the eruption of volcanic rocks during the mid-Early Cretaceous (130±2 to 124±2 Ma). The former is spatially, temporally and genetically associated with skarn gold-bearing mineralization (140.3±1.1 to 137.3±2.4 Ma). The recognition of these two igneous events invalidates previous models that proposed continuous magmatism and associated mineral deposits in the Middle–Lower Yangtze River Valley metallogenic belt.
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