锌矿
4.ISOTOPE GEOLOGY CHARACTERISTICS AND GENESIS OF THE QIWAN ZINC DEPOSITS, ZHEJIANG PROVINCE
5.A white or colored crystalline mineral, a variety of willemite, in which the zinc is partly replaced by manganese.
9.Phase transition of nano ZnS from wurtzite to rocksalt occurred at 16.0 GPa and 16.7 GPa for 10 nm and 3 nm sample,respectively,which were higher than that of the bulk materials.
10.Zinc2+ activates the flotation of silver-doped sphalerite while depresses the flotation of AgCl, Ag2SO4 and Ag2O.

