
What is an example of a common oxide mineral?
Answer
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Hint: We can say that a strong synthetic compound with a genuinely clear cut substance organization and a particular crystal design that happens normally in unadulterated form is a mineral. Eight components represent a large portion of the vital parts of minerals, because of their wealth in the crust.
Complete answer:
We have to know that an oxide mineral is any normally occurring inorganic compound with a structure dependent on close-packed atoms of oxygen in which more modest, positive charged metal or different particles happen in interstices. We have to know that oxides are recognized from other oxygen-bearing species like the silicates, borates, and carbonates, which have a promptly quantifiable group consisting of oxygen particles covalently attached to an atom of another component.
We have to know that the oxide mineral class remembers those minerals for which the oxide anion $\left( {{O^{2 - }}} \right)$is attached to at least one metal compound. We can say the hydroxide-bearing minerals are normally remembered for the oxide class. We can also say that the minerals with complex anion groups like the silicates, sulfates, carbonates and phosphates are classed independently.
We can give the examples of some common oxide minerals as ilmenite, hematite, magnetite, goethite, franklinite, nichrome, and chromite.
An example of a common oxide mineral is hematite.
Note:
We have to understand that rocks are nothing but aggregates of one mineral (or) more than one mineral. We have to know that ores are minerals which contain high concentrations of a specific element which is metal. We can say gems are also minerals that possess an ornamental value.
Complete answer:
We have to know that an oxide mineral is any normally occurring inorganic compound with a structure dependent on close-packed atoms of oxygen in which more modest, positive charged metal or different particles happen in interstices. We have to know that oxides are recognized from other oxygen-bearing species like the silicates, borates, and carbonates, which have a promptly quantifiable group consisting of oxygen particles covalently attached to an atom of another component.
We have to know that the oxide mineral class remembers those minerals for which the oxide anion $\left( {{O^{2 - }}} \right)$is attached to at least one metal compound. We can say the hydroxide-bearing minerals are normally remembered for the oxide class. We can also say that the minerals with complex anion groups like the silicates, sulfates, carbonates and phosphates are classed independently.
We can give the examples of some common oxide minerals as ilmenite, hematite, magnetite, goethite, franklinite, nichrome, and chromite.
An example of a common oxide mineral is hematite.
Note:
We have to understand that rocks are nothing but aggregates of one mineral (or) more than one mineral. We have to know that ores are minerals which contain high concentrations of a specific element which is metal. We can say gems are also minerals that possess an ornamental value.
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