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- W3122333438 endingPage "103995" @default.
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- W3122333438 abstract "Thermochronology has become an increasingly effective tool to reveal the post-mineralization uplift and exhumation history of ore deposits. In this paper, we studied the exhumation history and preservation conditions of the Xiuwacu tungsten-molybdenite deposit (resource: 24,000 t Mo and 23,000 t WO3), which is located on the southern Yidun Terrane (SYT), Eastern Tibetan Plateau. At Xiuwacu, both the eastern and western ore zones contain quartz-vein-type orebodies in the K-feldspar, greisen, and silicic alteration zones. The orebodies distributed in a northwestward trend along regional faults, with ore minerals including mainly molybdenite, scheelite, chalcopyrite, and pyrite. The mineralization at Xiuwacu occurred in 86–82 Ma, coeval with the emplacement of the ore-causative Xiuwacu porphyry monzogranite. The deposit likely underwent rapid cooling from 750 − 800 °C (magmatic zircon U-Pb age) to ~ 300 °C during 90–86 Ma (molybdenite Re-Os mineralization age). After that, the temperature slowly and continuously cooled to ~ 180 °C from the Late Cretaceous to 25 Ma, and then rapidly cooled to ~ 125 °C in 25–17 Ma, and eventually to 125–60 °C during 17–5 Ma (apatite fission-track ages; n = 8). The thermochronologic history of the Xiuwacu intrusive complex was reconstructed by inverse modelling based on the apatite fission-track ages and lengths. There was 6426–6915 m (average 6650 m) uplift, while only 1982–2471 m (average 2200 m) exhumation. Considering the depth of current exploration and typical depth of granitoid-related W-Mo mineralization, we infer that there is still great potential to discover concealed W-Mo orebodies beneath the current mining level at Xiuwacu." @default.
- W3122333438 created "2021-02-01" @default.
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- W3122333438 date "2021-05-01" @default.
- W3122333438 modified "2023-10-18" @default.
- W3122333438 title "Preservation of Xiuwacu W-Mo deposit and its constraint on the uplifting history of Eastern Tibetan Plateau" @default.
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- W3122333438 doi "https://doi.org/10.1016/j.oregeorev.2021.103995" @default.
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