A classic example of a mineral with a basic structure consisting of single tetrahedra linked by atoms of other elements is olivine.

Here's why:

* Tetrahedra: Olivine's fundamental building block is the silicate tetrahedron (SiO4)4-. This is a pyramid-shaped structure with a silicon atom at the center and four oxygen atoms at the corners.

* Linked by Other Elements: In olivine, these individual tetrahedra are linked together by magnesium (Mg) and iron (Fe) atoms. These cations sit between the tetrahedra, forming strong ionic bonds that hold the structure together.

This arrangement creates a relatively simple but robust structure that is characteristic of many silicate minerals.

Additional Examples:

While olivine is a common example, other minerals with this basic structure include:

* Garnet: Contains a variety of cations (like magnesium, calcium, iron, manganese, aluminum) linking the tetrahedra.

* Spinel: Features aluminum cations linking the tetrahedra.

Remember, this is just one type of silicate mineral structure. Many other variations exist with more complex arrangements of tetrahedra and linking elements.