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.
主要以类质同象存在于闪锌矿中,少量以硫矿等独
矿物形式存在于矿床
氧化带，是风化淋滤过程中形成
生矿物。
矿(绿色或橘色)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.
主要以类质同象存在于闪锌矿中,少量以硫矿等独矿物形式存在于矿床氧化带，是风化淋滤过程中形成生矿物。
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