There are some independent minerals of Cd, which are secondary minerals formed during weathering and leaching, such as greenockite, otavite and oxides of Cd in the oxidized zone of the deposit.
镉主要以类质同象
闪锌矿中,少量镉以硫镉矿等独
矿物形式矿床的氧
带，
淋滤过程中形成的镉的次生矿物。
There are some independent minerals of Cd, which are secondary minerals formed during weathering and leaching, such as greenockite, otavite and oxides of Cd in the oxidized zone of the deposit.
镉主要以类质同象闪锌矿中,少量镉以硫镉矿等独矿物形式矿床的氧带，淋滤过程中形成的镉的次生矿物。
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