Massive sulfide Cu-Zn deposit of Hongtoushan type which occurs in Archeozoic granitic greenstone terrain in Qinyuan area of Liaoning possesses unique geochemical characteristics.

• 产于辽宁省清原地区太古宙花岗-绿岩地体中的红透山式块状硫化物铜锌矿床,具有独特的地球化学特征。