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• W1732564837 endingPage "417" @default.
• W1732564837 startingPage "409" @default.
• W1732564837 abstract "Abstract Although the term orogenic gold deposit has been widely accepted for all gold-only lode-gold deposits, with the exception of Carlin-type deposits and rare intrusion-related gold systems, there has been continuing debate on their genesis. Early syngenetic models and hydrothermal models dominated by meteoric fluids are now clearly unacceptable. Magmatic-hydrothermal models fail to explain the genesis of orogenic gold deposits because of the lack of consistent spatially – associated granitic intrusions and inconsistent temporal relationships. The most plausible, and widely accepted, models involve metamorphic fluids, but the source of these fluids is hotly debated. Sources within deeper segments of the supracrustal successions hosting the deposits, the underlying continental crust, and subducted oceanic lithosphere and its overlying sediment wedge all have their proponents. The orogenic gold deposits of the giant Jiaodong gold province of China, in the delaminated North China Craton, contain ca. 120 Ma gold deposits in Precambrian crust that was metamorphosed over 2000 million years prior to gold mineralization. The only realistic source of fluid and gold is a subducted oceanic slab with its overlying sulfide-rich sedimentary package, or the associated mantle wedge. This could be viewed as an exception to a general metamorphic model where orogenic gold has been derived during greenschist- to amphibolite-facies metamorphism of supracrustal rocks: basaltic rocks in the Precambrian and sedimentary rocks in the Phanerozoic. Alternatively, if a holistic view is taken, Jiaodong can be considered the key orogenic gold province for a unified model in which gold is derived from late-orogenic metamorphic devolatilization of stalled subduction slabs and oceanic sediments throughout Earth history. The latter model satisfies all geological, geochronological, isotopic and geochemical constraints but the precise mechanisms of auriferous fluid release, like many other subduction-related processes, are model-driven and remain uncertain." @default.
• W1732564837 created "2016-06-24" @default.
• W1732564837 creator A5060053337 @default.
• W1732564837 creator A5063944243 @default.
• W1732564837 date "2016-05-01" @default.
• W1732564837 modified "2023-10-17" @default.
• W1732564837 title "The giant Jiaodong gold province: The key to a unified model for orogenic gold deposits?" @default.
• W1732564837 cites W1025143415 @default.
• W1732564837 cites W1492904818 @default.
• W1732564837 cites W1531882999 @default.
• W1732564837 cites W1748073762 @default.
• W1732564837 cites W1827364463 @default.
• W1732564837 cites W1949220332 @default.
• W1732564837 cites W1965559270 @default.
• W1732564837 cites W1966185813 @default.
• W1732564837 cites W1966218310 @default.
• W1732564837 cites W1966431820 @default.
• W1732564837 cites W1969598356 @default.
• W1732564837 cites W1972349245 @default.
• W1732564837 cites W1973086765 @default.
• W1732564837 cites W1974064297 @default.
• W1732564837 cites W1975988467 @default.
• W1732564837 cites W1976848297 @default.
• W1732564837 cites W1977878142 @default.
• W1732564837 cites W1980951510 @default.
• W1732564837 cites W1984118119 @default.
• W1732564837 cites W1986013659 @default.
• W1732564837 cites W1987645149 @default.
• W1732564837 cites W1989945922 @default.
• W1732564837 cites W1993523237 @default.
• W1732564837 cites W1993865247 @default.
• W1732564837 cites W1994093446 @default.
• W1732564837 cites W1995442541 @default.
• W1732564837 cites W1996586016 @default.
• W1732564837 cites W1996756941 @default.
• W1732564837 cites W2003158547 @default.
• W1732564837 cites W2005925547 @default.
• W1732564837 cites W2006466583 @default.
• W1732564837 cites W2007088963 @default.
• W1732564837 cites W2007139925 @default.
• W1732564837 cites W2008587842 @default.
• W1732564837 cites W2010129653 @default.
• W1732564837 cites W2011169560 @default.
• W1732564837 cites W2012359517 @default.
• W1732564837 cites W2016343665 @default.
• W1732564837 cites W2017529476 @default.
• W1732564837 cites W2019618011 @default.
• W1732564837 cites W2020507877 @default.
• W1732564837 cites W2024762872 @default.
• W1732564837 cites W2025567962 @default.
• W1732564837 cites W2026021257 @default.
• W1732564837 cites W2028972894 @default.
• W1732564837 cites W2029988187 @default.
• W1732564837 cites W2036001304 @default.
• W1732564837 cites W2036059154 @default.
• W1732564837 cites W2036848227 @default.
• W1732564837 cites W2038202477 @default.
• W1732564837 cites W2039228109 @default.
• W1732564837 cites W2041600017 @default.
• W1732564837 cites W2046590164 @default.
• W1732564837 cites W2051327484 @default.
• W1732564837 cites W2054244741 @default.
• W1732564837 cites W2054690551 @default.
• W1732564837 cites W2055394521 @default.
• W1732564837 cites W2057477615 @default.
• W1732564837 cites W2060230400 @default.
• W1732564837 cites W2060245822 @default.
• W1732564837 cites W2064232883 @default.
• W1732564837 cites W2064431901 @default.
• W1732564837 cites W2069718490 @default.
• W1732564837 cites W2072761602 @default.
• W1732564837 cites W2075901285 @default.
• W1732564837 cites W2076116164 @default.
• W1732564837 cites W2077684298 @default.
• W1732564837 cites W2078151478 @default.
• W1732564837 cites W2078316814 @default.
• W1732564837 cites W2081151322 @default.
• W1732564837 cites W2081537955 @default.
• W1732564837 cites W2083005035 @default.
• W1732564837 cites W2083808432 @default.
• W1732564837 cites W2090553280 @default.
• W1732564837 cites W2094895748 @default.
• W1732564837 cites W2098832267 @default.
• W1732564837 cites W2102727961 @default.
• W1732564837 cites W2106844742 @default.
• W1732564837 cites W2113504390 @default.
• W1732564837 cites W2118707213 @default.
• W1732564837 cites W2119607233 @default.
• W1732564837 cites W2133763977 @default.
• W1732564837 cites W2139573553 @default.
• W1732564837 cites W2139665334 @default.
• W1732564837 cites W2143326753 @default.
• W1732564837 cites W2150058503 @default.
• W1732564837 cites W2151595992 @default.
• W1732564837 cites W2153952174 @default.
• W1732564837 cites W2154295153 @default.
• W1732564837 cites W2155349595 @default.
• W1732564837 cites W2183427072 @default.

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