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• W2019949618 endingPage "787" @default.
• W2019949618 startingPage "764" @default.
• W2019949618 abstract "Uranium–Pb (zircon) ages are linked with geochemical data for porphyry intrusions associated with giant porphyry Cu–Au systems at Oyu Tolgoi to place those rocks within the petrochemical framework of Devonian and Carboniferous rocks of southern Mongolia. In this part of the Gurvansayhan terrane within the Central Asian Orogenic Belt, the transition from Devonian tholeiitic marine rocks to unconformably overlying Carboniferous calc-alkaline subaerial to shallow marine volcanic rocks reflects volcanic arc thickening and maturation. Radiogenic Nd and Pb isotopic compositions (εNd(t) range from + 3.1 to + 7.5 and 206Pb/204Pb values for feldspars range from 17.97 to 18.72), as well as low high-field strength element (HFSE) contents of most rocks (mafic rocks typically have < 1.5% TiO2) are consistent with magma derivation from depleted mantle in an intra-oceanic volcanic arc. The Late Devonian and Carboniferous felsic rocks are dominantly medium- to high-K calc-alkaline and characterized by a decrease in Sr/Y ratios through time, with the Carboniferous rocks being more felsic than those of Devonian age. Porphyry Cu–Au related intrusions were emplaced in the Late Devonian during the transition from tholeiitic to calc-alkaline arc magmatism. Uranium–Pb (zircon) geochronology indicates that the Late Devonian pre- to syn-mineral quartz monzodiorite intrusions associated with the porphyry Cu–Au deposits are ~ 372 Ma, whereas granodiorite intrusions that post-date major shortening and are associated with less well-developed porphyry Cu–Au mineralization are ~ 366 Ma. Trace element geochemistry of zircons in the Late Devonian intrusions associated with the porphyry Cu–Au systems contain distinct Th/U and Yb/Gd ratios, as well as Hf and Y concentrations that reflect mixing of magma of distinct compositions. These characteristics are missing in the unmineralized Carboniferous intrusions. High Sr/Y and evidence for magma mixing in syn- to late-mineral intrusions distinguish the Late Devonian rocks associated with giant Cu–Au deposits from younger magmatic suites in the district." @default.
• W2019949618 created "2016-06-24" @default.
• W2019949618 creator A5044548903 @default.
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• W2019949618 creator A5076559229 @default.
• W2019949618 date "2011-04-01" @default.
• W2019949618 modified "2023-10-17" @default.
• W2019949618 title "U–Pb (zircon) and geochemical constraints on the age, origin, and evolution of Paleozoic arc magmas in the Oyu Tolgoi porphyry Cu–Au district, southern Mongolia" @default.
• W2019949618 cites W1964909252 @default.
• W2019949618 cites W1964976672 @default.
• W2019949618 cites W1966256034 @default.
• W2019949618 cites W1968749260 @default.
• W2019949618 cites W1970621049 @default.
• W2019949618 cites W1972077181 @default.
• W2019949618 cites W1972158246 @default.
• W2019949618 cites W1972256629 @default.
• W2019949618 cites W1984923148 @default.
• W2019949618 cites W1996553891 @default.
• W2019949618 cites W1997694024 @default.
• W2019949618 cites W1997710040 @default.
• W2019949618 cites W2001019604 @default.
• W2019949618 cites W2001266646 @default.
• W2019949618 cites W2003323528 @default.
• W2019949618 cites W2004791239 @default.
• W2019949618 cites W2007105153 @default.
• W2019949618 cites W2008456126 @default.
• W2019949618 cites W2011016972 @default.
• W2019949618 cites W2011584645 @default.
• W2019949618 cites W2013025728 @default.
• W2019949618 cites W2013222877 @default.
• W2019949618 cites W2016848882 @default.
• W2019949618 cites W2024321144 @default.
• W2019949618 cites W2034223887 @default.
• W2019949618 cites W2036255513 @default.
• W2019949618 cites W2038775297 @default.
• W2019949618 cites W2039689699 @default.
• W2019949618 cites W2042266298 @default.
• W2019949618 cites W2044394940 @default.
• W2019949618 cites W2045459201 @default.
• W2019949618 cites W2048579003 @default.
• W2019949618 cites W2053335831 @default.
• W2019949618 cites W2054816670 @default.
• W2019949618 cites W2055500440 @default.
• W2019949618 cites W2057164831 @default.
• W2019949618 cites W2057620806 @default.
• W2019949618 cites W2058762125 @default.
• W2019949618 cites W2059497122 @default.
• W2019949618 cites W2059817759 @default.
• W2019949618 cites W2065065857 @default.
• W2019949618 cites W2075655861 @default.
• W2019949618 cites W2081673195 @default.
• W2019949618 cites W2092346956 @default.
• W2019949618 cites W2094264745 @default.
• W2019949618 cites W2103463307 @default.
• W2019949618 cites W2104692056 @default.
• W2019949618 cites W2105272296 @default.
• W2019949618 cites W2106142284 @default.
• W2019949618 cites W2106344463 @default.
• W2019949618 cites W2108971421 @default.
• W2019949618 cites W2110218619 @default.
• W2019949618 cites W2111713335 @default.
• W2019949618 cites W2112435406 @default.
• W2019949618 cites W2119695127 @default.
• W2019949618 cites W2119991869 @default.
• W2019949618 cites W2122963132 @default.
• W2019949618 cites W2127705220 @default.
• W2019949618 cites W2131128362 @default.
• W2019949618 cites W2131545507 @default.
• W2019949618 cites W2131772367 @default.
• W2019949618 cites W2136852838 @default.
• W2019949618 cites W2139788788 @default.
• W2019949618 cites W2151455489 @default.
• W2019949618 cites W2153415850 @default.
• W2019949618 cites W2153769775 @default.
• W2019949618 cites W2157099954 @default.
• W2019949618 cites W2160590991 @default.
• W2019949618 cites W2163661859 @default.
• W2019949618 cites W2165495127 @default.
• W2019949618 cites W2168363532 @default.
• W2019949618 cites W2321801909 @default.
• W2019949618 cites W2325019720 @default.
• W2019949618 cites W4232130546 @default.
• W2019949618 cites W4232366222 @default.
• W2019949618 cites W4237162788 @default.
• W2019949618 cites W4253807186 @default.
• W2019949618 doi "https://doi.org/10.1016/j.gr.2010.11.012" @default.
• W2019949618 hasPublicationYear "2011" @default.
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