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- W2034892768 abstract "The East Qinling–Dabie molybdenum belt is part of a larger East–West trending metallogenic belt in eastern China. Most of the molybdenum deposits occur as porphyry or porphyry–skarn type, but there are also some vein type deposits. Following systematic Re–Os dating of molybdenite from 13 deposits and comparisons with two previously dated deposits, we have recognized that the molybdenum mineralization in the East Qinling–Dabie belt was developed during hydrothermal activity linked to magmatism and the emplacement of granitoid stocks. Three pulses of granitoid magmatism and Mo mineralization are recognized corresponding to significant tectonic events in the East Qinling–Dabie belt. Vein type deposits dated at 233–221 Ma were formed in detachment fractures, indicating localized extension within the collisional setting of the North China and Yangtze Cratons. I-type and transitional I- and S-type granites and related mineralization dated at 148–138 Ma may have formed part of a continental magmatic arc, with widespread magmatism and back-arc extension caused by subduction of the Izanagi or Paleopacific plate beneath the Eurasian continent in a WNW–ESE direction in the Late Jurassic–Early Cretaceous. Both S-type and transitional S- and I-type granite-associated porphyry molybdenum deposits dated at 131–112 Ma are part of an extensive mineralization event throughout East China that can be ascribed to regional large-scale lithospheric thinning, delamination and thermal erosion." @default.
- W2034892768 created "2016-06-24" @default.
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- W2034892768 date "2008-09-01" @default.
- W2034892768 modified "2023-10-06" @default.
- W2034892768 title "Tectonic implications from Re–Os dating of Mesozoic molybdenum deposits in the East Qinling–Dabie orogenic belt" @default.
- W2034892768 cites W1509458422 @default.
- W2034892768 cites W1840936257 @default.
- W2034892768 cites W1973125903 @default.
- W2034892768 cites W1979840893 @default.
- W2034892768 cites W1981278331 @default.
- W2034892768 cites W1985745494 @default.
- W2034892768 cites W1986092846 @default.
- W2034892768 cites W1987759514 @default.
- W2034892768 cites W1988341539 @default.
- W2034892768 cites W1991132092 @default.
- W2034892768 cites W1994209198 @default.
- W2034892768 cites W1996784988 @default.
- W2034892768 cites W1998481085 @default.
- W2034892768 cites W2000795509 @default.
- W2034892768 cites W2001119618 @default.
- W2034892768 cites W2002042103 @default.
- W2034892768 cites W2003454252 @default.
- W2034892768 cites W2005925547 @default.
- W2034892768 cites W2010906549 @default.
- W2034892768 cites W2011250343 @default.
- W2034892768 cites W2013579065 @default.
- W2034892768 cites W2015726616 @default.
- W2034892768 cites W2016511472 @default.
- W2034892768 cites W2020092856 @default.
- W2034892768 cites W2021112336 @default.
- W2034892768 cites W2025597990 @default.
- W2034892768 cites W2027316964 @default.
- W2034892768 cites W2031839367 @default.
- W2034892768 cites W2035451444 @default.
- W2034892768 cites W2036936240 @default.
- W2034892768 cites W2037234776 @default.
- W2034892768 cites W2042173471 @default.
- W2034892768 cites W2043657636 @default.
- W2034892768 cites W2044496537 @default.
- W2034892768 cites W2047314228 @default.
- W2034892768 cites W2048261322 @default.
- W2034892768 cites W2049907150 @default.
- W2034892768 cites W2052779241 @default.
- W2034892768 cites W2052964693 @default.
- W2034892768 cites W2053422899 @default.
- W2034892768 cites W2058193023 @default.
- W2034892768 cites W2061559926 @default.
- W2034892768 cites W2063006645 @default.
- W2034892768 cites W2063754919 @default.
- W2034892768 cites W2066857758 @default.
- W2034892768 cites W2067480884 @default.
- W2034892768 cites W2068726160 @default.
- W2034892768 cites W2071462919 @default.
- W2034892768 cites W2073326270 @default.
- W2034892768 cites W2077516804 @default.
- W2034892768 cites W2081673871 @default.
- W2034892768 cites W2082270747 @default.
- W2034892768 cites W2083238138 @default.
- W2034892768 cites W2098570811 @default.
- W2034892768 cites W2104177181 @default.
- W2034892768 cites W2106158114 @default.
- W2034892768 cites W2106844742 @default.
- W2034892768 cites W2112797646 @default.
- W2034892768 cites W2114111971 @default.
- W2034892768 cites W2130335288 @default.
- W2034892768 cites W2141514627 @default.
- W2034892768 cites W2145091879 @default.
- W2034892768 cites W2154141422 @default.
- W2034892768 cites W2154886810 @default.
- W2034892768 cites W2163696442 @default.
- W2034892768 cites W2164886516 @default.
- W2034892768 cites W2603964733 @default.
- W2034892768 cites W3149938784 @default.
- W2034892768 doi "https://doi.org/10.1016/j.gca.2008.06.027" @default.
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