Theoretical model of phyllosilicates

The theoretical model of phyllosilicates describes their structure as layers of linked silicate sheets. These sheets consist of silicon and oxygen atoms arranged in a hexagonal pattern, forming a stable, two-dimensional network. Between these layers, other ions or molecules, such as magnesium or aluminum, can reside, acting like glue or spacers. This layered arrangement explains their characteristic properties, like flexibility and ability to absorb water, and helps scientists understand their behavior in natural processes and industrial applications. The model provides a detailed, structural understanding of how these minerals form, function, and interact within Earth’s crust.