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• W3202531738 endingPage "104506" @default.
• W3202531738 startingPage "104506" @default.
• W3202531738 abstract "The metal and sulfur fertility of granite magmas that formed in post-subduction settings, the key processes that led to their contrasting associated polymetallic mineral deposits, and their post-subduction source remain obscure. The Yidun Terrane, eastern Tibet, extends for 500 km and can be divided into the northern Yidun Terrane (NYT) and southern Yidun Terrane (SYT) based on distinctive magmatic source affinities and related mineral deposits. The NYT has several 103–93 Ma granite plutons and associated magmatic-hydrothermal vein-type Sn–Pb–Zn–Ag polymetallic deposits, such as the giant Xiasai deposit. In contrast, the SYT granites host the Xiuwacu porphyry Mo–W deposit (88–84 Ma) and several porphyry or porphyry–skarn-type Cu–Mo deposits (85–78 Ma), such as Relin, Hongshan and Tongchanggou. The contrasting nature of the causative Cretaceous post-subduction granites and their source is determined from their whole-rock and isotope geochemistry, zircon trace-element concentrations, and biotite and amphibole mineral chemistry. Based on these parameters, the NYT Sn–Pb–Zn–Ag deposits are associated with highly fractionated, reduced ilmenite-series granites derived from a relatively dry magma that formed via mixing between amphibolite-derived and greywacke- and orthogneiss-derived metasomatized crustal melts. In contrast, the SYT Mo–W deposits are associated with strongly- to moderately-evolved and fractionated, oxidized intermediate-series granites. The SYT Cu–Mo deposits are related to more hydrous and less fractionated magnetite-series granites. The granites associated with both Mo–W and Cu–Mo deposits in the SYT were generated by partial melting of metasomatized ancient mafic-intermediate lower continental-crust with variable contributions of metasomatized mantle components. However, there is only evidence for the presence of garnet as a residual phase in the magmatic source of the SYT Cu–Mo-bearing granites. The different magma sources were important in determining the redox state of the Yidun granite magmas, providing a fundamental control on the behaviour of metals and sulfur in fractionating melts and dictating the contrasting polymetallic compositions of causative magmatic-hydrothermal fluids and resultant mineral deposits. The source regions of the granites are thus the primary control on the spatial distribution of the Sn–Pb–Zn–Ag, Mo–W, and Cu–Mo belts in the Yidun Terrane. Although not derived during subduction, as for most Cenozoic porphyry systems, the Yidun deposits are indirectly related to subduction via the metasomatism and fertilization of the mantle lithosphere and lower crust during the earlier subduction phase. The anomalous preservation of Cretaceous porphyry systems in the Yidun Terrane relates to their proximity to the margin of the Yangtze Craton, whose thick buoyant lithosphere inhibited exhumation and erosion." @default.
• W3202531738 created "2021-10-11" @default.
• W3202531738 creator A5017604949 @default.
• W3202531738 creator A5045912046 @default.
• W3202531738 creator A5063944243 @default.
• W3202531738 creator A5053303262 @default.
• W3202531738 date "2021-12-01" @default.
• W3202531738 modified "2023-10-15" @default.
• W3202531738 title "Redox conditions, compositional parameters, and indirect subduction-related source of Cretaceous Sn and Cu–Mo fertile post-subduction granites in the Yidun Terrane of eastern Tibet" @default.
• W3202531738 cites W1524950519 @default.
• W3202531738 cites W1578122124 @default.
• W3202531738 cites W1797283169 @default.
• W3202531738 cites W1830506594 @default.
• W3202531738 cites W1884854517 @default.
• W3202531738 cites W1968681946 @default.
• W3202531738 cites W1969859799 @default.
• W3202531738 cites W1971685925 @default.
• W3202531738 cites W1973923863 @default.
• W3202531738 cites W1974957554 @default.
• W3202531738 cites W1977650828 @default.
• W3202531738 cites W1991589759 @default.
• W3202531738 cites W2006372142 @default.
• W3202531738 cites W2009985436 @default.
• W3202531738 cites W2014495917 @default.
• W3202531738 cites W2022859730 @default.
• W3202531738 cites W2026270769 @default.
• W3202531738 cites W2028048720 @default.
• W3202531738 cites W2029182942 @default.
• W3202531738 cites W2030023077 @default.
• W3202531738 cites W2031928338 @default.
• W3202531738 cites W2032340654 @default.
• W3202531738 cites W2035185474 @default.
• W3202531738 cites W2036174339 @default.
• W3202531738 cites W2044226470 @default.
• W3202531738 cites W2048593294 @default.
• W3202531738 cites W2049111683 @default.
• W3202531738 cites W2052044676 @default.
• W3202531738 cites W2054513641 @default.
• W3202531738 cites W2054653182 @default.
• W3202531738 cites W2056283375 @default.
• W3202531738 cites W2057218369 @default.
• W3202531738 cites W2063948745 @default.
• W3202531738 cites W2067270209 @default.
• W3202531738 cites W2070024898 @default.
• W3202531738 cites W2073474967 @default.
• W3202531738 cites W2081507714 @default.
• W3202531738 cites W2081673871 @default.
• W3202531738 cites W2083915255 @default.
• W3202531738 cites W2084975451 @default.
• W3202531738 cites W2085181355 @default.
• W3202531738 cites W2086984328 @default.
• W3202531738 cites W2087795440 @default.
• W3202531738 cites W2090953932 @default.
• W3202531738 cites W2095298264 @default.
• W3202531738 cites W2095348500 @default.
• W3202531738 cites W2100411277 @default.
• W3202531738 cites W2102290079 @default.
• W3202531738 cites W2107506859 @default.
• W3202531738 cites W2110609253 @default.
• W3202531738 cites W2111184969 @default.
• W3202531738 cites W2117561599 @default.
• W3202531738 cites W2123260607 @default.
• W3202531738 cites W2130671654 @default.
• W3202531738 cites W2136178989 @default.
• W3202531738 cites W2138522501 @default.
• W3202531738 cites W2143722440 @default.
• W3202531738 cites W2145826681 @default.
• W3202531738 cites W2154628848 @default.
• W3202531738 cites W2160816054 @default.
• W3202531738 cites W2162017737 @default.
• W3202531738 cites W2162974904 @default.
• W3202531738 cites W2181312688 @default.
• W3202531738 cites W2199739494 @default.
• W3202531738 cites W2279160735 @default.
• W3202531738 cites W2313729349 @default.
• W3202531738 cites W2315324142 @default.
• W3202531738 cites W2438447823 @default.
• W3202531738 cites W2461226224 @default.
• W3202531738 cites W2583214058 @default.
• W3202531738 cites W2588552471 @default.
• W3202531738 cites W2591115756 @default.
• W3202531738 cites W2594260502 @default.
• W3202531738 cites W2742718310 @default.
• W3202531738 cites W2789599720 @default.
• W3202531738 cites W2789835083 @default.
• W3202531738 cites W2790120547 @default.
• W3202531738 cites W2791086831 @default.
• W3202531738 cites W2791974310 @default.
• W3202531738 cites W2800288578 @default.
• W3202531738 cites W2911530812 @default.
• W3202531738 cites W2924622270 @default.
• W3202531738 cites W2939813251 @default.
• W3202531738 cites W2954278936 @default.
• W3202531738 cites W2964065245 @default.
• W3202531738 cites W2966151060 @default.
• W3202531738 cites W3007424236 @default.
• W3202531738 cites W3111908487 @default.
• W3202531738 cites W3137661253 @default.

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