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- W2383118676 abstract "The ore-bearing rocks in the Yangshan gold deposit, Wenxian, Gansu, are a sequence of Devonian carbonaceous-siliceous-argillaceous sediments, which contains abundant framboidal pyrite with As anomaly (～0.15% As). Orebodies occur as tectonic lenses or pods equidistantly along the secondary fractured zone or bedding-parallel shear zone in a fault belt. In mineralized sulfide in the early-middle phase, Au occurs as invisible gold in As-bearing pyrite and arsenopyrite. As-bearing pyrite displays overgrowth zoning. The Au carriers mainly occur as micro-disseminations along the schistose zone. Microscopic gold grains are visible in metal sulfide-quartz crushed veins formed in the middle and late phases. Plagiogranite porphyry is crustal anatectic granite formed by multiple intrusions. H, O, and S isotope and fluid inclusion data indicate that ore fluids consist mainly of meteoric water mixed with small amount of magmatic water. Thus it follows that the Yangshan gold deposit is a superlarge Carlin and Carlin-like type polygenetic gold deposit with magma-telescoped, sedimentary and tectonically and hydrothermally modified features." @default.
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- W2383118676 date "2006-01-01" @default.
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- W2383118676 title "Genesis and types of the Yangshan superlarge micro-disseminated gold deposit, Wenxian, Gansu, China" @default.
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