sulfidid

Sulfidid is a rare mineral belonging to the sulfide mineral group. It was first discovered in 1999 in the Khibina alkaline complex in Kola Peninsula, Russia. The mineral is named after its chemical composition, which includes sulfur and various metals such as nickel, iron, and cobalt.

Sulfidid is characterized by its metallic luster and dark color, ranging from black to dark gray. It typically forms small, anhedral crystals or massive aggregates. The mineral is often associated with other sulfide minerals like pentlandite and chalcopyrite.

The chemical formula of sulfidid is (Ni,Fe)S2, indicating that it is a nickel-iron sulfide. The mineral's structure is similar to that of pyrite, with sulfur atoms forming a cubic arrangement and metal atoms occupying the interstitial sites.

Sulfidid is of interest to mineralogists and geologists due to its rarity and the unique conditions under which it forms. It is typically found in magmatic sulfide deposits, where it precipitates from cooling magma. The mineral's presence can provide valuable information about the geological processes and conditions that led to its formation.

Despite its scientific significance, sulfidid is not known to have any significant industrial applications. Its rarity and the challenges associated with its extraction make it an uncommon mineral in the world of mining and metallurgy. However, its study contributes to our understanding of the Earth's geological history and the formation of sulfide deposits.