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• W2616532041 endingPage "162" @default.
• W2616532041 startingPage "141" @default.
• W2616532041 abstract "THIS Gold in 2000volume is organized around a classification of hypogene gold deposits that emphasizes their tectonic setting and relative time of formation compared to their host rocks and other gold deposit types (e.g., Sawkins, 1972, 1990; Groves et al., 1998; Kerrich et al., 2000). The temporal division of orogenic gold deposits into Archean, Proterozoic, and Phanerozoic follows closely the recently published classification of orogenic gold deposits (Groves et al., 1998) which incorporates the previously identified “mesothermal” gold deposits. The newly recognized intrusion-related and sedex gold deposits represent new gold deposit classes even though their exact genetic classification remains open, with more research considered a priority. Proterozoic Au-only and Cu-Au-(Fe) deposits are also a relatively recently recognized class of structurally controlled epigenetic gold deposits. Particularly, the origin and classification of Cu-Au-(Fe) deposits (e.g., Olympic Dam) remains equivocal, as pointed out by Partington and Williams (2000). In fact, Kerrich et al. (2000) discuss the anorogenic iron oxide copper-gold deposits as one of six world-class gold deposit classes. Low- and high-sulfidation and hot spring epithermal gold deposits are dealt with as one genetic gold class. Alkalic epithermal and porphyry gold deposits are dealt with as a separate gold deposit class owing to their specific host-rock association and element enrichment (e.g., Mo, F, Be, Hg, W, and Sn).The gold deposit classes are described from both industry and academic points of view, with emphasis on a balanced account of the descriptive geology, genetic interpretations, exploration significance, as well as open questions and future research avenues. The volume contains 13 papers covering 10 major classes of gold deposits and three summary papers, and was presented as a Society of Economic Geologists-sponsored short course held November 10 and 11, 2000, at Lake Tahoe, Nevada.Orogenic gold ores are associated with regionally metamorphosed terranes of all ages (Kerrich and Cassidy, 1994) and are spatially linked to subduction-related thermal processes (Kerrich and Wyman, 1990)(Fig. 1). These metal concentrations formed during compressional to transpressional deformation processes at convergent plate margins in accretionary (oceanic-continental plate interaction) and collisional (continental-continental collision) orogens (i.e., Bohlke, 1982; Groves et al., 1998). In both cases hydrated marine sedimentary and volcanic rocks have been added to continental margins over a long period of collision (10 to >100 Ma). Accretionary or peripheral orogens contain gold deposits in the Archean of Australia, Canada, Africa, India, and Brazil and the Mesozoic and Cenozoic gold fields of western North America, i.e., the famous Mother Lode belt. Collisional or internal orogens contain gold deposits in the Proterozoic of Australia, North America, West Africa, and Brazil, and the famous Phanerozoic gold fields in the Variscan, Appalachian, and Alpine regions of North America and Europe. In Phanerozoic orogenic gold deposits, subduction- related thermal events, episodically raising geothermal gradients within the hydrated accretionary sequences, initiate and drive long-distance hydrothermal fluid migration." @default.
• W2616532041 created "2017-05-26" @default.
• W2616532041 creator A5024040110 @default.
• W2616532041 creator A5042372703 @default.
• W2616532041 date "2000-01-01" @default.
• W2616532041 modified "2023-10-10" @default.
• W2616532041 title "Fluid Chemistry of Orogenic Lode Gold Deposits and Implications for Genetic Models" @default.
• W2616532041 cites W136974534 @default.
• W2616532041 cites W1492000624 @default.
• W2616532041 cites W1964174750 @default.
• W2616532041 cites W1965179608 @default.
• W2616532041 cites W1970614852 @default.
• W2616532041 cites W1972342782 @default.
• W2616532041 cites W1972845188 @default.
• W2616532041 cites W1974064297 @default.
• W2616532041 cites W1975792409 @default.
• W2616532041 cites W1975988467 @default.
• W2616532041 cites W1977794195 @default.
• W2616532041 cites W1978299137 @default.
• W2616532041 cites W1983061564 @default.
• W2616532041 cites W1983430242 @default.
• W2616532041 cites W1984881578 @default.
• W2616532041 cites W1985827600 @default.
• W2616532041 cites W1986290753 @default.
• W2616532041 cites W1988830113 @default.
• W2616532041 cites W1992123305 @default.
• W2616532041 cites W1996321458 @default.
• W2616532041 cites W1997746397 @default.
• W2616532041 cites W2001790553 @default.
• W2616532041 cites W2003365107 @default.
• W2616532041 cites W2006858514 @default.
• W2616532041 cites W2009020736 @default.
• W2616532041 cites W2009123615 @default.
• W2616532041 cites W2010261459 @default.
• W2616532041 cites W2010980831 @default.
• W2616532041 cites W2013603991 @default.
• W2616532041 cites W2015848058 @default.
• W2616532041 cites W2017468132 @default.
• W2616532041 cites W2018209051 @default.
• W2616532041 cites W2019618011 @default.
• W2616532041 cites W2020516660 @default.
• W2616532041 cites W2021893756 @default.
• W2616532041 cites W2022128851 @default.
• W2616532041 cites W2025023772 @default.
• W2616532041 cites W2026295157 @default.
• W2616532041 cites W2027789468 @default.
• W2616532041 cites W2028617991 @default.
• W2616532041 cites W2028915875 @default.
• W2616532041 cites W2028917031 @default.
• W2616532041 cites W2030938679 @default.
• W2616532041 cites W2031910622 @default.
• W2616532041 cites W2036183472 @default.
• W2616532041 cites W2037321146 @default.
• W2616532041 cites W2038367243 @default.
• W2616532041 cites W2040525887 @default.
• W2616532041 cites W2041508176 @default.
• W2616532041 cites W2042712602 @default.
• W2616532041 cites W2044297606 @default.
• W2616532041 cites W2044402799 @default.
• W2616532041 cites W2045235745 @default.
• W2616532041 cites W2056982746 @default.
• W2616532041 cites W2058642293 @default.
• W2616532041 cites W2059867089 @default.
• W2616532041 cites W2059900164 @default.
• W2616532041 cites W2066822004 @default.
• W2616532041 cites W2068073788 @default.
• W2616532041 cites W2071622819 @default.
• W2616532041 cites W2071697085 @default.
• W2616532041 cites W2075901285 @default.
• W2616532041 cites W2076047591 @default.
• W2616532041 cites W2076521030 @default.
• W2616532041 cites W2076863471 @default.
• W2616532041 cites W2078316814 @default.
• W2616532041 cites W2078320350 @default.
• W2616532041 cites W2078656065 @default.
• W2616532041 cites W2079041911 @default.
• W2616532041 cites W2079900150 @default.
• W2616532041 cites W2080999233 @default.
• W2616532041 cites W2081666993 @default.
• W2616532041 cites W2084157369 @default.
• W2616532041 cites W2085191160 @default.
• W2616532041 cites W2085532500 @default.
• W2616532041 cites W2087806970 @default.
• W2616532041 cites W2089322652 @default.
• W2616532041 cites W2093559711 @default.
• W2616532041 cites W2094316302 @default.
• W2616532041 cites W2095549129 @default.
• W2616532041 cites W2097873023 @default.
• W2616532041 cites W2098347203 @default.
• W2616532041 cites W2104335635 @default.
• W2616532041 cites W2105779189 @default.
• W2616532041 cites W2111372566 @default.
• W2616532041 cites W2111660215 @default.
• W2616532041 cites W2112037730 @default.
• W2616532041 cites W2115375715 @default.
• W2616532041 cites W2116792643 @default.
• W2616532041 cites W2119339013 @default.
• W2616532041 cites W2120270131 @default.

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