The preparation of zinc sulfate heptahydrate and copper sulfate pentahydrate from calcined zincblende was investigated.

用经高温煅烧后的闪石与稀硫酸反应制备七水硫酸和五水硫酸铜。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

石由黄铁、闪、然金、辉锑、砷黝铜、辉锑、辉锑银、雄黄、雌黄等成,为典型的低温热液合。

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.

镉主要以类质同象存在于闪中,少量镉以硫镉等独立形式存在于床的氧化带，是风化淋滤过程中形成的镉的次生。

The preparation of zinc sulfate heptahydrate and copper sulfate pentahydrate from calcined zincblende was investigated.

用经高温煅烧后矿石与稀硫酸反应制备七水硫酸和五水硫酸铜。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

矿石由黄铁矿、矿、自然金、辉锑矿、砷黝铜矿、辉锑矿、辉锑银矿、雄黄、雌黄等组成,为典型低温热液矿物组合。

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.

镉主要以类质同象在于矿中,少量镉以硫镉矿等独立矿物在于矿床氧化带，是风化淋滤过程中成镉次生矿物。

The preparation of zinc sulfate heptahydrate and copper sulfate pentahydrate from calcined zincblende was investigated.

用经高温煅烧后的闪锌石与稀硫酸反应制备七水硫酸锌和五水硫酸铜。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

石由铁、闪锌、自然金、、砷黝铜、、、、雌等组成,为典型的低温热液物组合。

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.

镉主要以类质同象存在于闪锌中,少量镉以硫镉等独立物形式存在于床的氧化带，是风化淋滤过程中形成的镉的次生物。

The preparation of zinc sulfate heptahydrate and copper sulfate pentahydrate from calcined zincblende was investigated.

用经高温煅烧后的闪锌石与稀反应制备七锌和五铜。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

石由黄铁、闪锌、自然金、辉锑、砷黝铜、辉锑、辉锑银、雄黄、雌黄等组成,为典型的低温热液物组合。

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.

镉主要以类质同象存在于闪锌,量镉以镉等独立物形式存在于床的氧化带，是风化淋滤过程形成的镉的次生物。

The preparation of zinc sulfate heptahydrate and copper sulfate pentahydrate from calcined zincblende was investigated.

用经高温煅烧后的石与稀硫酸反应制备七水硫酸和五水硫酸铜。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

石由黄铁、、自然金、辉锑、砷黝铜、辉锑、辉锑银、雄黄、雌黄等成,为典型的低温热液物。

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.

主要以类质同象存在于中,少量以硫等独立物形式存在于床的氧化带，是风化淋滤过程中形成的的次生物。

The preparation of zinc sulfate heptahydrate and copper sulfate pentahydrate from calcined zincblende was investigated.

用经高温煅烧后的闪锌石与稀硫酸反应制备七水硫酸锌和五水硫酸。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

石由黄铁、闪锌、自然金、锑、砷黝、锑、锑银、雄黄、雌黄,为典型的低温热液物合。

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.

镉主要以类质同象存在于闪锌中,少量镉以硫镉独立物形式存在于床的氧化带，是风化淋滤过程中形的镉的次生物。

The preparation of zinc sulfate heptahydrate and copper sulfate pentahydrate from calcined zincblende was investigated.

用经高温煅烧后的闪锌石与反应制备七水锌和五水铜。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

石由黄铁、闪锌、自然金、辉锑、砷黝铜、辉锑、辉锑银、雄黄、雌黄组成,为典型的低温热液物组合。

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.

镉主要以类质同象存在于闪锌中,少量镉以镉立物形式存在于床的氧化带，是风化淋滤过程中形成的镉的次生物。

The preparation of zinc sulfate heptahydrate and copper sulfate pentahydrate from calcined zincblende was investigated.

用经高煅烧后的闪锌矿石与稀硫酸反应制备七水硫酸锌和五水硫酸铜。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

矿石由黄铁矿、闪锌矿、自、锑矿、砷黝铜矿、锑矿、锑银矿、雄黄、雌黄等组成,为典型的低矿物组合。

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.

镉主要以类质同象存在于闪锌矿中,少量镉以硫镉矿等独立矿物形式存在于矿床的氧化带，是风化淋滤过程中形成的镉的次生矿物。

The preparation of zinc sulfate heptahydrate and copper sulfate pentahydrate from calcined zincblende was investigated.

用经高温煅烧后的闪石与稀反应制备七水和五水铜。

Ores consist of pyrite, blende, aurum, zinckenite, tennantite, antimonite, realgar, and orpiment, belong to typical Low-temperature minerals assemblage .

石由黄铁、闪、自然金、辉锑、砷黝铜、辉锑、辉锑银、雄黄、雌黄等组成,为典型的低温热液物组合。

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.

镉主要以类质同象存在于闪,少量镉以镉等独立物形式存在于床的氧化带，是风化淋滤过程形成的镉的次生物。