Origin and tectonic setting of the giant Duolong Cu-Au deposit, South Qiangtang Terrane, Tibet: Evidence from geochronology and geochemistry of Early Cretaceous intrusive rocks
We present a detailed regional geological investigation at Duolong.
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The ore-associated rocks formed by fractional crystallization of mantle-derived mafic melts and magma mixing of mantle-derived mafic melts and hybrid lower crust-derived felsic melts.
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The deposit formed on the ensialic forearc.
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