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• W2768737356 endingPage "587" @default.
• W2768737356 startingPage "569" @default.
• W2768737356 abstract "The newly discovered Daxintun Sb-Au deposit (Heilongjiang province, NE China) is located at the north-eastern margin of the Central Asian Orogenic Belt, and it is hosted by Neoproterozoic to Early-Cambrian two-mica schist and marble. The antimony-bearing minerals include stibnite, famatinite, tetrahedrite, boulangerite, freibergite, and minor andorite. Gold occurs largely as native gold microparticles (0.1–20 μm) with high fineness (974–983) accompanied by quartz, stibnite, calcite and pyrite. Fluid inclusions in ore-bearing quartz and calcite phases mainly comprise liquid–vapor and minor CO2-bearing three-phase types, and the gas phases contain CO2, CH4 and H2S. The Daxintun fluid inclusions homogenize at 111.8–353.4 °C and are of low salinity (0.53–12.51 wt% NaCl equiv.). The δ18OSMOW of the Daxintun quartz falls into a wide range (4.2‰–16.9‰), yet the δDSMOW falls into a narrow range (−108.0‰ to −87.3‰), suggesting that the ore-forming fluids formed from metamorphic fluids that mixed with meteoric water. The stibnite δ34S ranges between −0.9‰ and 5.1‰ (mean = 2.8‰). The stibnite has 206Pb/204Pb of 18.234–18.306, 207Pb/204Pb of 15.537–15.561 and 208Pb/204Pb of 38.103–38.227, implying a metamorphic fluid source. The conditions of gold and antimony precipitation are comprised of neutral pH and fluid mixing, with decreasing fS2 and fO2. Zircon U-Pb dating of the fine-grained Daxintun granite yields a Late-Jurassic age (154.0 ± 2.0 Ma), and the Daxintun diorite dike yields a weighted mean age of 122.1 ± 1.3 Ma. Stibnite Rb-Sr dating suggests that the Sb-Au mineralization has an age of approximately 152.8 ± 2.4 Ma. The observed ore deposit geology, as well as new data on the ore-forming fluids, H-O-S-Pb isotopes, and Rb-Sr geochronology, suggest that the Daxintun Sb-Au deposit is best described as an orogenic type gold deposit that formed during subduction of the Palaeo-Pacific and the Mongolia–Okhotsk Oceans during the Late-Jurassic." @default.
• W2768737356 created "2017-12-04" @default.
• W2768737356 creator A5006212782 @default.
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• W2768737356 date "2018-01-01" @default.
• W2768737356 modified "2023-10-03" @default.
• W2768737356 title "Geology, hydrothermal fluids, H-O-S-Pb isotopes, and Rb-Sr geochronology of the Daxintun orogenic gold deposit in Heilongjiang province, NE China" @default.
• W2768737356 cites W1051026135 @default.
• W2768737356 cites W1688431902 @default.
• W2768737356 cites W1892477717 @default.
• W2768737356 cites W1965524050 @default.
• W2768737356 cites W1965826523 @default.
• W2768737356 cites W1967827341 @default.
• W2768737356 cites W1969371403 @default.
• W2768737356 cites W1970439132 @default.
• W2768737356 cites W1970621049 @default.
• W2768737356 cites W1971733245 @default.
• W2768737356 cites W1982536542 @default.
• W2768737356 cites W1986117163 @default.
• W2768737356 cites W1988557437 @default.
• W2768737356 cites W1989318729 @default.
• W2768737356 cites W1993716912 @default.
• W2768737356 cites W1995897602 @default.
• W2768737356 cites W1997705537 @default.
• W2768737356 cites W2005925547 @default.
• W2768737356 cites W2010326351 @default.
• W2768737356 cites W2020973699 @default.
• W2768737356 cites W2021378803 @default.
• W2768737356 cites W2022286646 @default.
• W2768737356 cites W2024746457 @default.
• W2768737356 cites W2025236494 @default.
• W2768737356 cites W2025402991 @default.
• W2768737356 cites W2025493942 @default.
• W2768737356 cites W2033127801 @default.
• W2768737356 cites W2034428765 @default.
• W2768737356 cites W2038677898 @default.
• W2768737356 cites W2039405518 @default.
• W2768737356 cites W2039872199 @default.
• W2768737356 cites W2045041501 @default.
• W2768737356 cites W2045300556 @default.
• W2768737356 cites W2054366973 @default.
• W2768737356 cites W2055112659 @default.
• W2768737356 cites W2055164627 @default.
• W2768737356 cites W2059333429 @default.
• W2768737356 cites W2072011665 @default.
• W2768737356 cites W2075771303 @default.
• W2768737356 cites W2075901285 @default.
• W2768737356 cites W2077214987 @default.
• W2768737356 cites W2078320350 @default.
• W2768737356 cites W2078811057 @default.
• W2768737356 cites W2079598225 @default.
• W2768737356 cites W2081926628 @default.
• W2768737356 cites W2082258012 @default.
• W2768737356 cites W2084051225 @default.
• W2768737356 cites W2087806970 @default.
• W2768737356 cites W2089096123 @default.
• W2768737356 cites W2090757504 @default.
• W2768737356 cites W2091071952 @default.
• W2768737356 cites W2101108033 @default.
• W2768737356 cites W2102828314 @default.
• W2768737356 cites W2111660215 @default.
• W2768737356 cites W2112648202 @default.
• W2768737356 cites W2131542227 @default.
• W2768737356 cites W2134909530 @default.
• W2768737356 cites W2136349207 @default.
• W2768737356 cites W2145604970 @default.
• W2768737356 cites W2148239728 @default.
• W2768737356 cites W2148957284 @default.
• W2768737356 cites W2153952174 @default.
• W2768737356 cites W2169766597 @default.
• W2768737356 cites W2173601591 @default.
• W2768737356 cites W2223957627 @default.
• W2768737356 cites W2225969652 @default.
• W2768737356 cites W2229174120 @default.
• W2768737356 cites W2259771641 @default.
• W2768737356 cites W2567018470 @default.
• W2768737356 cites W2897983685 @default.
• W2768737356 cites W2995482781 @default.
• W2768737356 cites W3146972477 @default.
• W2768737356 cites W3149162803 @default.
• W2768737356 cites W4238080741 @default.
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• W2768737356 doi "https://doi.org/10.1016/j.oregeorev.2017.11.014" @default.
• W2768737356 hasPublicationYear "2018" @default.
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