answersLogoWhite

0

Isolated tetrahedra silicates do not link with other silicon or oxygen atoms

Ring Silicates form by sharing oxygen atoms

Single Chain Silicates form a chain when sharing oxygen atoms

Double Chain Silicates form when two or more single chains of tetrahedra bond to each other

Sheet Silicates form when each tetrahedron shares three of its oxygen atoms with other tetrahedra

Framework Silicates form when each tetrahedron is bonded to four other tetrahedras

:)

User Avatar

Wiki User

12y ago

What else can I help you with?

Continue Learning about Earth Science

What are the 6 main crystalline structures of silicate minerals?

The six main crystalline structures of silicate minerals are isolated tetrahedra, single chain, double chain, sheet, framework, and ring structures. Each structure is based on how the silicate tetrahedra are arranged and linked together in the mineral's crystal lattice.


If silicon bonded with three oxygen atoms how might the crystalline structures of silicate minerals?

If silicon is bonded to three oxygen atoms, it will form a silicate tetrahedron. Silicate minerals can have different crystalline structures depending on how these tetrahedra are arranged, such as in chains, sheets, or three-dimensional networks. This arrangement determines the physical properties of the mineral.


What factors affect the structures of silicate minerals as they are forming?

The temperature, pressure, and chemical composition of the surrounding environment can all influence the formation and structure of silicate minerals. Factors such as the cooling rate and the presence of other elements can also impact the crystalline structure that forms. Additionally, the length of time available for mineral growth can affect the final structure of the silicate mineral.


What is the grouping of silicate and non-silicate minerals based on?

The grouping of silicate and non-silicate minerals is based on whether they contain silicon and oxygen. Silicate minerals are divided into smaller groups based on their structure. Non-silicate minerals are didvided into smaller groups based on their composition.


How are silicate minerals different from non silicate minerals?

Silicates are found in just about every variety of rock, including sedimentary, igneous and metamorphic. The thing that differentiates silicates from other minerals is the presence of the element silicon in the matrix. It is silicon that silicate minerals are named for. Use link below to check out this huge family of minerals.

Related Questions

What are the six main crystalline structures of silicate minerals?

How magnetism can be useful for identifying minerals


What The six main crystalline structures of silicate minerals?

How magnetism can be useful for identifying minerals


What are the 6 main crystalline structures of silicate minerals?

The six main crystalline structures of silicate minerals are isolated tetrahedra, single chain, double chain, sheet, framework, and ring structures. Each structure is based on how the silicate tetrahedra are arranged and linked together in the mineral's crystal lattice.


If silicon bonded with three oxygen atoms how might the crystalline structures of silicate minerals?

If silicon is bonded to three oxygen atoms, it will form a silicate tetrahedron. Silicate minerals can have different crystalline structures depending on how these tetrahedra are arranged, such as in chains, sheets, or three-dimensional networks. This arrangement determines the physical properties of the mineral.


What are three common non silicate crystalline structures?

Non-silicate crystalline structures are tetrahedra, isolated, and chains.


Why non silicate minerals have wider variety of crystalline structures than silicate minerasls do?

Non-silicate minerals contain oxygen and native elements. They have metallic and non-metallic lusters, and are very common.


What are crystalline structures?

Non-silicate crystalline structures are tetrahedra, isolated, and chains.


Which are nonsillicate crystalline structures?

a double chain silicate is


What are the primary elements that connect the large silicate structures to one another in the silicate minerals?

Turtles Bruh


What factors affect the structures of silicate minerals as they are forming?

The temperature, pressure, and chemical composition of the surrounding environment can all influence the formation and structure of silicate minerals. Factors such as the cooling rate and the presence of other elements can also impact the crystalline structure that forms. Additionally, the length of time available for mineral growth can affect the final structure of the silicate mineral.


How are minerals divided?

Minerals are divided into groups based on their chemical composition and crystalline structure. The two main groups are silicate minerals, which are made of silicon and oxygen, and non-silicate minerals, which are composed of other elements. Within these groups, minerals are further classified based on their specific properties and characteristics.


How many minerals are silicate minerals?

90% of minerals are silicate.