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.

用经高温煅烧后的闪锌矿石与稀反应制备七水锌和五水。

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、自然金、辉锑矿、砷黝矿、辉锑矿、辉锑银矿、雄黄、雌黄等组成,为典型的低温热液矿物组合。

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.

镉主要以类质在于闪锌矿中,少量镉以镉矿等独立矿物形式在于矿床的氧化带，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、雌黄等组成,为典型的低温热液组合。

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中,少量镉以硫镉等独立存在于床的氧化带，是风化淋滤过程中成的镉的次生。

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.

用经高温煅烧后的闪锌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 .

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中,少量镉以硫镉等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 .

石由黄、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。

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.

要以类质同象存在于锌中,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.

用经高温煅烧后的矿石与稀硫酸反应制备七水硫酸水硫酸铜。

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,为典型的低温热液矿物组合。

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.

镉主要以类质同象存在矿中,少量镉以硫镉矿等独立矿物形式存在矿床的氧化带，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锌矿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 .

矿铁矿、闪锌矿、自然金、辉锑矿、砷黝铜矿、辉锑矿、辉锑银矿、雄、雌等组成,为典型的低温热液矿物组合。

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.

镉主质同象存在于闪锌矿中,少量镉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。