《Table 3 Results of electron probe analysis of sulfosalt mineral (boulangerite) replacing coarse-gra

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《"The Zhaxikang Vein-type Pb-Zn-Ag-Sb Deposit in Himalayan Orogen, Tibet: Product by Overprinting and Remobilization Processes during Post-collisional Period"》

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Brecciated coarse-grained sphalerite that formed during period A is dark black（Fig.6 b1）and is free of chalcopyrite，whereas the later-formed sphalerite contains numerous chalcopyrite droplets.This brecciated sphalerite is also overprinted by later fluids，causing increase of Cu and loss of Fe（Fig.12 and Fig.13）and a systematic decrease in sphalerite Fe concentrations from core to rim（Table 4），which presents dark black to nigger-brown to light yellow.