黄铜矿

The sulfide assemlage consists largely of pyrrhotite, pentlandite, chalcopyrite, and pyrite.

硫化物集体大部由磁黄铁矿 、 镍黄铁矿 、 黄铜矿及黄铁矿组成。

Associated minerals are mainly magnetite and ilmenite, subordinately pyrite and rarely chalcopyrite.

主要伴生矿物为磁铁矿、钛铁矿， 少量黄铁矿和微量黄铜矿。

While chalcopyrite adsorbs gold most weakly with its adsorption capacity 9 % only.

吸附性相对最弱的是黄铜矿，吸附量仅为9%。

The cathodic reduction is stronger and plays an important role for the dissolution of chalcopyrite.

黄铜矿的阴极还原反应较强烈，且对黄铜矿氧化浸出具有重要意义。

Most of them are highly silicified and sometimes mineralized with pyrite and chalcopyrite.

大部分的扭折条带遭受强烈的硅化作用，有时还具有矿化现象，并含黄铁矿和黄铜矿。