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

于闪锌矿中,少量
以硫
矿等独立矿物形

于矿床
氧化带,是风化淋滤过程中形


次生矿物。
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

于闪锌矿中,少量
以硫
矿等独立矿物形

于矿床
氧化带,是风化淋滤过程中形


次生矿物。
It is thought that greenockite is a seconday (supergenic) mineral, but there has been found primary greenockite in the Niujiaotang cadmium-zinc deposit in Guizhou.
贵州牛角塘
锌矿床中既有次生硫
矿

,也发现了原生硫
矿。
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