FeAl2Si4O10OH2

FeAl2Si4O10OH2 is a complex mineral belonging to the group of tectosilicates. It was first discovered in the Allende meteorite, a carbonaceous chondrite, and has since been identified in other meteorites and lunar samples. The mineral is characterized by its unique chemical composition, which includes iron (Fe), aluminum (Al), silicon (Si), oxygen (O), and hydrogen (H). Its crystal structure is complex, with a framework of silicon-oxygen tetrahedra and aluminum-oxygen octahedra, interspersed with iron and hydrogen atoms.

FeAl2Si4O10OH2 is notable for its occurrence in extraterrestrial environments, suggesting it may have formed under conditions different from those on Earth. Its discovery and study contribute to our understanding of the chemical processes that occur in the solar system, particularly in the early stages of planetary formation. The mineral's name is derived from its chemical formula, reflecting its composition and structure.

Research on FeAl2Si4O10OH2 is ongoing, with scientists investigating its properties and potential implications for planetary science. Its study may provide insights into the conditions under which it formed and the processes that led to its incorporation into meteorites and lunar samples.