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• W2017110729 endingPage "58" @default.
• W2017110729 startingPage "29" @default.
• W2017110729 abstract "Abstract The North Atlantic craton of southwestern Greenland hosts several orogenic gold occurrences, although, to date, none is in production. Four gold provinces are distinguished and include Godthabsfjord, Tasiusarsuaq, Paamiut, and Tartoq. In the Godthabsfjord gold province, the hypozonal gold occurrences are aligned along the major ca. 2660–2600 Ma Ivinnguit fault. Orogenic gold mineralization correlates temporally with, and is related to, ductile deformation along this first-order structure. The northern part of the Tasiusarsuaq gold province is characterized by small hypozonal gold occurrences that are controlled by 2670–2610 Ma folds and shear zones. Auriferous fluids were focused into the structures in both gold provinces during west-directed accretion of the Kapisilik terrane (2650–2580 Ma) to the already amalgamated terranes of the North Atlantic craton. In the southern part of the Tasiusarsuaq gold province, hypozonal gold mineralization is hosted in back-thrusts (Sermilik prospect) and thrusts (Bjornesund prospect) that formed at 2740 Ma and 2860–2830 Ma, respectively. The deformation is related to the ca. 2850 Ma accretion of the Sioraq block and the Tasiusarsuaq terrane, and the 2800–2700 Ma accretion of the Tasiusarsuaq terrane and the Faeringehavn and Tre Brodre terranes. Mesozonal orogenic gold mineralization is hosted in an accretionary complex in the Paamiut and Tartoq gold provinces. Gold occurrences cluster over a strike extent of approx. 40 km in thrusts and complex strike-slip settings in lateral ramps. The timing of the E-vergent terrane accretion in both areas is unknown, and could either be at ca. 2850 Ma or 2740 Ma. In the eastern part of the Paamiut gold province, quartz veins and associated alteration zones were overprinted by granulite facies metamorphism and show evidence for partial melting. These outermost parts of the accretionary complex were involved in burial-exhumation tectonics during crustal accretion. Mainly three different orogenic stages related to gold mineralization are distinguished in the North Atlantic craton between ca. 2850 Ma and 2610 Ma. These are generally accretionary tectonic episodes, and gold mineralization is hosted either in reactivated fault systems between terranes or accretionary complex structures along the deformed cratonic margin. The larger orogenic gold occurrences formed at ca. 2740–2600 Ma that appears to be a period of orogenic gold mineralization globally, although significant gold resources in the North Atlantic craton have yet to be identified." @default.
• W2017110729 created "2016-06-24" @default.
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• W2017110729 creator A5069229597 @default.
• W2017110729 date "2013-10-01" @default.
• W2017110729 modified "2023-10-17" @default.
• W2017110729 title "Gold occurrences of the Archean North Atlantic craton, southwestern Greenland: A comprehensive genetic model" @default.
• W2017110729 cites W1525942184 @default.
• W2017110729 cites W1964970129 @default.
• W2017110729 cites W1966014029 @default.
• W2017110729 cites W1967347520 @default.
• W2017110729 cites W1969092428 @default.
• W2017110729 cites W1976133378 @default.
• W2017110729 cites W1976185588 @default.
• W2017110729 cites W1977050044 @default.
• W2017110729 cites W1980787557 @default.
• W2017110729 cites W1982841476 @default.
• W2017110729 cites W1985295636 @default.
• W2017110729 cites W1990470414 @default.
• W2017110729 cites W1994018460 @default.
• W2017110729 cites W2005925547 @default.
• W2017110729 cites W2007380260 @default.
• W2017110729 cites W2007848912 @default.
• W2017110729 cites W2011040748 @default.
• W2017110729 cites W2011169560 @default.
• W2017110729 cites W2011954957 @default.
• W2017110729 cites W2013093639 @default.
• W2017110729 cites W2017367788 @default.
• W2017110729 cites W2019875617 @default.
• W2017110729 cites W2023737199 @default.
• W2017110729 cites W2024674294 @default.
• W2017110729 cites W2029599884 @default.
• W2017110729 cites W2030347901 @default.
• W2017110729 cites W2037544442 @default.
• W2017110729 cites W2044568109 @default.
• W2017110729 cites W2045857800 @default.
• W2017110729 cites W2059553419 @default.
• W2017110729 cites W2059825259 @default.
• W2017110729 cites W2066313292 @default.
• W2017110729 cites W2068807428 @default.
• W2017110729 cites W2075901285 @default.
• W2017110729 cites W2078151478 @default.
• W2017110729 cites W2078316814 @default.
• W2017110729 cites W2078811057 @default.
• W2017110729 cites W2080391252 @default.
• W2017110729 cites W2081537955 @default.
• W2017110729 cites W2082729095 @default.
• W2017110729 cites W2084281827 @default.
• W2017110729 cites W2085191160 @default.
• W2017110729 cites W2085606826 @default.
• W2017110729 cites W2088934812 @default.
• W2017110729 cites W2090666494 @default.
• W2017110729 cites W2092296914 @default.
• W2017110729 cites W2094640762 @default.
• W2017110729 cites W2094895748 @default.
• W2017110729 cites W2095473629 @default.
• W2017110729 cites W2098509806 @default.
• W2017110729 cites W2098832267 @default.
• W2017110729 cites W2101464572 @default.
• W2017110729 cites W2111343877 @default.
• W2017110729 cites W2115364092 @default.
• W2017110729 cites W2116477609 @default.
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• W2017110729 cites W2146381706 @default.
• W2017110729 cites W2147847344 @default.
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• W2017110729 cites W2155512758 @default.
• W2017110729 cites W2157045821 @default.
• W2017110729 cites W2164031340 @default.
• W2017110729 cites W2165003604 @default.
• W2017110729 cites W4238080741 @default.
• W2017110729 doi "https://doi.org/10.1016/j.oregeorev.2013.01.019" @default.
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