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- W2361384127 abstract "The Matou lindgrenite deposit in Anhui Province is a porphyry deposit in the AnqingChizhou area of the Middle-Lower Yangtze River Valley,Eastern China.Two Re-Os isotopic dating on molybdenites collected from the granodiorite porphyry ores and the Fentou Formation sandy slate ores yield a Re-Os model age of 148.6Ma±2.1Ma and 150.2Ma±2.7Ma respectively,with an average age of 149.2Ma±3.2Ma,showing good agreement with the zircon U-Pb age of granodiorite porphyry(147Ma±2Ma).Therefore,149.2Ma±3.2Ma can represent the forming age of the Matou lindgrenite deposit.This ore-forming age is different from isotopic dating results(145Ma~125Ma)provided by earlier workers in the area.The Re content in molybdenites of Matou lindgrenite deposit is 134×10-6 and 421×10-6,indicating that the ore-forming material is mainly originated from the mantle.The determination of the rock-forming ages and ore-forming ages(in late Jurassic)of Matou lindgrenite deposit and other polymetallic deposits in the Middle-Lower Yangtze River Valley suggests these deposits may be formed under the same geodynamics setting of the tectonic transition from the EW trend tectonic domain to the NNE trend tectonic domain in east China." @default.
- W2361384127 created "2016-06-24" @default.
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- W2361384127 date "2014-01-01" @default.
- W2361384127 modified "2023-09-28" @default.
- W2361384127 title "Re-Os ISOTOPIC DATING OF MOLYBDENITE FROM THE MATOU IINDGRENITE DEPOSIT FROM CHIZHOU AREA IN THE SOUTH OF ANHUI PROVINCE AND ITS GEOLOGICAL IMPLICATIONS" @default.
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