sphalerite

Its crystal structure is cubic, like that for sphalerite and diamond.

Sphalerite or zinc sulfide is also, common in the region.

Whereas the sphalerite for zinc production is the minor source.

The sphalerite is an important source of zinc throughout the ore belts.

The technical terminology might be "sphalerite in a matrix of pyrite".

This is the main form of zinc found in nature, where it mainly occurs as the mineral sphalerite.

It is often found with the minerals sphalerite, calcite and fluorite.

The more stable cubic form is known also as zinc blende or sphalerite.

Zinc blende (two words) is another name for the mineral "sphalerite".

The silver concentration in sphalerite is 946 g/t.

Pabstite can also be found associated with galena, cassiterite and sphalerite.

Other products from the mine are chalcocite, chalcopyrite, galena, and sphalerite.

The geologic setting that it occurs in is in the replacement of Sphalerite.

It was used to recover a sphalerite concentrate from tailings, produced using gravity concentration.

It is a grey-black crystalline solid semi-metal with a sphalerite structure.

It has a defect sphalerite (cubic form of ZnS) structure.

These minerals are accompanied by sphalerite, pyrite and chalcopyrite.

Greenockite occurs with other sulfide minerals such as sphalerite and galena.

Some specimens have a red iridescence within the gray-black crystals; these are called "ruby sphalerite."

It also occurred alongside large quantities of sphalerite, the principal ore of Zinc.

The most exploited zinc ore is sphalerite, a zinc sulfide.

In 1857, sphalerite, barite and stibnite were discovered and mined for several decades.

Primary ore minerals are silver-bearing galena and sphalerite; traces of native silver have also been found.

Junitoite occurs in fractures through pods of sphalerite.

The sphalerite polymorph of rubidium chloride is extremely rare, resulting in few structural studies.