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Carbonates- ex. Dolomite

Halides- ex. Halite

Native elements- ex. Silver

Oxides- ex. Corundum

Sulfates- ex. Gypsum

Sulfides- ex. Galena

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Solon Thompson

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What are six classes of non silicates?

Carbonates- ex. Dolomite Halides- ex. Halite Native elements- ex. Silver Oxides- ex. Corundum Sulfates- ex. Gypsum Sulfides- ex. Galena


What are the two major mineral grouped?

Silicates and non-silicates.


What is another word for non silicates?

Minerals that are not silicates can be referred to as "non-silicate minerals" or "non-silicate geological compounds."


What are the two most common kinds of minerals?

Silicates and non-silicates.


What is the difference ferromagnesian and non-ferromagnesian silicates?

Ferromagnesian silicates contain iron and magnesium in their composition, which gives them a dark color and high density. Non-ferromagnesian silicates do not contain iron and magnesium, resulting in lighter colors and lower densities. Ferromagnesian silicates tend to be denser and have higher melting points compared to non-ferromagnesian silicates.


What are two big groups of minerals called?

Silicates and non-silicates are the two big groups of minerals. Silicates are the most abundant mineral group on Earth and contain silicon and oxygen, while non-silicates include minerals such as carbonates, sulfides, oxides, and native elements.


What most common mineral group is broken into the subgroups of ferromagnesian and non ferromagnesian?

The most common mineral group that is broken into the subgroups of ferromagnesian and non-ferromagnesian is the silicate mineral group. Ferromagnesian silicates contain iron and/or magnesium, while non-ferromagnesian silicates do not contain these elements. Examples of ferromagnesian silicates include olivine and pyroxene, while examples of non-ferromagnesian silicates include feldspar and quartz.


What are the six main types of crystalline structures in silicate materials?

The six main types of crystalline structures in silicate materials are framework silicates (e.g., quartz), sheet silicates (e.g., muscovite), chain silicates (e.g., pyroxenes), single tetrahedra (e.g., olivine), double tetrahedra (e.g., garnet), and ring silicates (e.g., beryl).


What are the 2 main mineral groups and their subgroups?

The two main mineral groups are silicates and non-silicates. Silicates further divide into subclasses such as tectosilicates, inosilicates, sorosilicates, and cyclosilicates. Non-silicates include groups like carbonates, sulfides, oxides, and halides, among others.


What are Non-Silicates?

Well It is basically ( in this case) oxygen without silicon or oxygen


Describe the six main crystalline structures of silicate minerals?

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 :)


What are the 2 main families of rock-forming minerals?

The two main families of rock-forming minerals are silicates and non-silicates. Silicates, which include minerals like quartz and feldspar, are the most abundant group and contain silicon and oxygen in their structure. Non-silicates, such as carbonates, oxides, and sulfates, do not include silicon and oxygen in their basic composition and comprise a diverse range of minerals. Together, these families contribute to the formation of igneous, sedimentary, and metamorphic rocks.