tephroite-fayalite series
Quick Summary
The tephroite-fayalite series refers to a group of minerals within the broader olivine family. Tephroite, a manganese silicate (Mn₂SiO₄), forms a solid solution with fayalite, an iron silicate (Fe₂SiO₄). This means that in the molecular structure, manganese can be completely replaced by iron, and vice versa, creating a continuous range of compositions between the two end-members.12
These minerals are typically found in iron-manganese ore deposits, skarns, and metamorphosed manganese-rich sediments. While olivines in general are common rock-forming minerals, tephroite and fayalite are more specifically associated with these particular geological environments.12
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