"http://wiki.answers.com/Q/What_is_the_osi_ratio_in_a_silicate_sheet"
2.5
A sheet-like silicate structure refers to a mineral arrangement where silicate tetrahedra are stacked in a sheet-like fashion. Examples include minerals like mica and clay minerals, where the tetrahedra are arranged in continuous flat layers. These structures give the minerals their characteristic properties, such as cleavage and low hardness.
3/1
No, feldspar is not a sheet silicate. It belongs to the tectosilicate group, which forms a framework structure rather than sheets like those found in phyllosilicates.
A structural type of silicate mineral in which flat sheets are formed by the sharing of three of the four oxygen atoms in each tetrahedron with neighboring tetrahedrons. Also known as layer silicate; sheet mineral; sheet silicate.
Yes, muscovite is a silicate mineral. It belongs to the phyllosilicate group, which consists of minerals with a sheet-like structure. Muscovite is a common mica mineral that is composed of potassium, aluminum, silicon, oxygen, and hydrogen.
A silicate sheet has one cleavage plane, which allows it to split easily along this flat surface. This cleavage plane is a result of the structure of silicon and oxygen atoms arranged in sheets within the mineral.
Hornblende has a double chain silicate structure. This structure consists of pairs of linked tetrahedra that form continuous chains in two dimensions.
No, the ratio of silicon to oxygen can vary among different silicate minerals. The overall structure and composition of the mineral will determine the specific ratio of silicon to oxygen present in that mineral.
Yes, Muscovite is a silicate mineral. It belongs to the group of sheet silicates and is composed of aluminum, potassium, and silicon. It is commonly found in granite and metamorphic rocks.
3
Mica is a group of sheet silicate minerals (e.x of micas : Biotite, muscovite)