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

用经烧后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,为典型低热液物组合。

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氧化带，是风化淋滤过程中形成镉次生物。

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、、银、雄、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.

镉类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锌矿石与稀硫酸反应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.

主要类质同象存在于闪锌矿中,少硫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的次生矿物。

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

经高温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，风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、锌矿、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.

镉主要以类质同象于锌矿中,少量镉以硫镉矿等独立矿物形于矿床氧化带，是风化淋滤过程中形成镉次生矿物。

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 .

石由黄铁、闪锌、自然金、辉、砷黝铜、辉、辉、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于闪锌矿,少量镉以硫镉矿等独立矿物式存在于矿床的氧化带，是风化淋滤过成的镉的次生矿物。

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于闪锌矿,少量镉以硫镉矿等独立矿物形式存在于矿床的氧化带，是风化淋滤形成的镉的次生矿物。