Russian scientists made an important discovery about minerals deep in the earth. They discovered two types of ferropericlase, one of the essential minerals that make up our planet’s lower mantle. This discovery could significantly aid the search for diamond deposits.
Ferropericlase is a mineral that plays an important role in the formation of diamonds. It reveals two different types, one that is rich in magnesium and nickel and forms in the lower mantle, and the other that is poor in nickel and forms in the upper mantle. This discovery made it possible to understand the origin and diversity of ferropericlase, which could be useful in the exploration of diamond deposits.
Diamonds are often found in certain rocks called kimberlites. These rocks bring diamonds to the surface from deep in the mantle. It has previously been difficult to explain the diversity of ferropericlase composition, but now this discovery could help improve diamond prospecting methods, including the use of ferropericlase as a tracer.
Source: Ferra
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