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The elements that make up a mineral

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silicate minerals and non silicate minerals

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90% of minerals are silicate.

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Silicate and non-silicate minerals are grouped based on their chemical composition. Silicate minerals contain silica tetrahedra, while non-silicate minerals do not have this structure. Silicate minerals are the most abundant group of minerals on Earth.

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silicate and non silicate minerals

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Silicate minerals are a group of minerals that contain oxygen and silicon as their primary constituents. Examples of silicate minerals include quartz, feldspar, mica, and amphibole. These minerals are the most abundant in the Earth's crust.

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The two major groups of minerals are silicate minerals and non-silicate minerals. Silicate minerals contain silicon and oxygen, while non-silicate minerals do not contain these elements. Silicate minerals make up the vast majority of Earth's crust.

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Non-silicate minerals don't contain silicon and oxygen in tandem; silicate minerals do.

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The silicon-oxygen tetrahedron is the building block of silicate minerals. The word "silicate" means the compound contains silicon in some form.

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Jasper is a silicate mineral. It belongs to the quartz group of minerals and is composed primarily of silicon dioxide, which is a common component of silicate minerals.

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Silicate minerals are a class of minerals that make up over 90% of the Earth's crust. They contain silicon and oxygen as their primary components, typically combined with other elements like aluminum, iron, magnesium, or calcium. Silicate minerals are characterized by their tetrahedral structure, where one silicon atom is surrounded by four oxygen atoms.

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The Earth's crust is made mostly of silicate minerals. Silicate minerals are the most abundant minerals in the Earth's crust and are composed of silicon and oxygen atoms.

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Quartz, Feldspar, Muscovite, Biotite are among most common silicate minerals.

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No, non-silicate minerals do not contain silicon. Silicate minerals are the most common group of minerals on Earth and they are composed of silicon and oxygen atoms. Non-silicate minerals are composed of other elements, such as carbonates, sulfates, or native elements like gold and silver.

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A non-silicate mineral is a mineral that does not contain silicon and oxygen as its primary components. Examples of non-silicate minerals include calcite (calcium carbonate) and halite (sodium chloride). These minerals have diverse chemical compositions and properties compared to silicate minerals.

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Carbonate minerals contain carbonate groups (CO3^2-) in their chemical structure, while silicate minerals contain silicate tetrahedra (SiO4^4-) as their primary building blocks. Carbonate minerals tend to be more soluble in water and react more readily with acids compared to silicate minerals. Additionally, carbonate minerals typically have a non-silicate mineral composition, while silicate minerals are the most abundant group of minerals on Earth.

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Only 10% of the Earth's crust is composed of non-silicate minerals. Examples of non-silicate minerals are barringerite, nickel phosphide, taenite and suessite.

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Silicate minerals are can make up more than 90 percent of the earth's crust, the rest is made up of nonsilicate minerals, 10 percent.

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Raul A. Deju has written:

'Regional hydrology fundamentals' -- subject(s): Hydrology

'Surface properties of silicate minerals' -- subject(s): Silicate minerals

'A chemical interpretation of surface phenomena in silicate minerals' -- subject(s): Silicate minerals, Surface chemistry

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non-silicate and silicate minerals

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The two main families of rock forming minerals are silicate minerals and non-silicate minerals. Silicate minerals are the most abundant and include minerals such as quartz and feldspar, while non-silicate minerals include groups like carbonates and sulfates.

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The most common class of minerals is the silicate minerals, which make up over 90% of the Earth's crust. Silicate minerals contain silicon and oxygen atoms in their chemical structure, and they form various types of minerals such as quartz, feldspar, and mica.

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The mica group of silicate minerals cleave into thin sheets. O REALLY!!!!!!

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

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Yes, non-silicate minerals can still contain oxygen. For example, carbonates such as calcite and dolomite are non-silicate minerals that contain oxygen along with carbon and other elements.

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Silicate minerals are minerals that contain silicon and oxygen in their chemical makeup, while non-silicate minerals do not contain these elements. Silicate minerals are the most common type of minerals found on Earth, making up about 90% of the Earth's crust, while non-silicate minerals make up the remaining 10%. Silicate minerals have a structure based on silica tetrahedra, which consist of a silicon atom surrounded by four oxygen atoms.

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The silicate group. The silicate group includes these minerals; quartz, feldspars, and micas.

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The major family of rock-forming minerals is the silicate minerals. These minerals are made up of silicon and oxygen atoms, often combined with other elements like aluminum, iron, and magnesium. Some examples of silicate minerals include quartz, feldspar, and mica.

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silicon, oxygen, iron and magnesium

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These are known as silicate minerals or silicates.

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nonsilicate and silicate minerals

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Quartz and feldspars are the most common silicate minerals of the crust.

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Yes. The majority of rocks from any period of earth's history will be predominantly made of silicate minerals.

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The silicate group of minerals comprise the largest percentage of the Earth's crust. Silicate minerals include quartz, feldspars, and micas.

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All silicate minerals are composed of silicon and oxygen atoms arranged in a tetrahedral structure. These tetrahedra can be linked together in various formations to create different silicate mineral groups, such as sheet silicates, framework silicates, and chain silicates. Silicate minerals are the most abundant group of minerals in the Earth's crust.

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Yes, cleavage in silicate minerals is related to the arrangement of silicon-oxygen tetrahedra in their structure. The presence of planes of weakness along specific crystallographic directions in the silicate structure allows for cleavage to occur. This cleavage in silicate minerals is typically observed along planes parallel to the tetrahedral sheets in their structure.

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They all contain the silicon-oxygen tetrahedron.

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

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Lithium is a non-silicate mineral. It is typically found in minerals such as spodumene, lepidolite, and petalite, which belong to the silicate mineral group.

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Yes, emerald is a silicate mineral. It belongs to the beryl family of minerals, which is composed of beryllium aluminum silicate.

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Silicate minerals are the most abundant in Earth's crust and mantle because silicon and oxygen, the main components of silicate minerals, are the most abundant elements in the Earth's crust. This abundance of silicon and oxygen leads to the formation of silicate minerals through various geological processes, making them the most common type of minerals found in the Earth's crust and mantle.

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Neso-, soro-, cyclo-, ino-, phyllo- and tectosilicates are all the groups of silicate minerals.

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nonsilicate and silicate minerals

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the basic block of the silicate minerals are formed from rocks.

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No, carbonate does not contain silicate. Carbonate minerals are composed of carbon and oxygen ions, while silicate minerals are composed of silicon and oxygen ions.

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No, iron ore is not a silicate mineral. Iron ore is typically composed of iron oxides, such as hematite and magnetite, which are not silicate minerals. Silicate minerals are minerals that contain silica, oxygen, and other elements like silicon and aluminum.

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