👉 Paleocrystalline is a type of crystalline structure formed by the interaction between two or more crystals. It occurs in both solid and liquid forms, often occurring at the boundaries between different minerals. In the context of crystallography, it refers to the arrangement of atoms within a crystal lattice, as opposed to the chemical bonding between atoms. Paleocrystalline is distinguished from other types of crystalline structures such as monoclinic, orthorhombic, and
