Chain silicates, also known as inosilicates, are a group of minerals characterized by their unique structure of silicate tetrahedra. These shapes interlock to form chains, with variations including single, double, or even more complex formations.
The arrangement of these chains plays a critical role in determining the physical properties of the mineral. Two common types of chain silicates are Pyroxenes and Amphiboles.
- Pyroxenes: These are single-chain silicates that are significant constituents in many igneous and metamorphic rocks.
- Amphiboles: These minerals have double chains and exhibit a wider range of chemical compositions and structures.
The diversity in the chain configurations of silicates allows for a wide array of mineral properties, making chain silicates crucial to geological studies and applications.