mafisemöykynmineraalit
Mafisemöykynmineraalit, a term derived from Finnish, refers to a group of silicate minerals characterized by their abundance in magnesium and iron. These minerals are typically dark in color, ranging from black to dark green and brown, and possess a relatively high density. Their crystal structures are often complex, with many mafic minerals exhibiting a prismatic or bladed habit.
The formation of mafisemöykynmineraalit is intrinsically linked to the cooling and solidification of magma. They are
Common examples of mafisemöykynmineraalit include olivine, pyroxenes (like augite and enstatite), and amphiboles (such as hornblende).