Schreibersite is a rare mineral that was first discovered by a German mineralogist named Adolph von Schreibers in 1866. This mineral is typically found in meteorites and is usually composed of iron, nickel, and phosphorus. Although there are no commonly accepted synonyms for Schreibersite, it is sometimes referred to as "phosphide of iron" due to its chemical composition. Other possible terms used to describe this mineral include "nickel-iron phosphide" and "iron-nickel phosphide." Regardless of its name, Schreibersite is an important mineral for scientists studying the origins of our solar system since it is predominately found in meteorites.