Iron Silica Membrane Structures at the Nanoscale
iron silica is one of the most abundant mineral forms in Earth’s solid interior. It is a member of the olivine series, which consists of olivine (Fe2SiO4) and its soluble end-members forsterite and fayalite, along with members of the forsterite-fayalite series and the intermediate members in the olivine series, including… Continue reading