bromide
One example of a mineral that contains the CO3 group is calcite. Calcite is a common mineral that is composed of calcium carbonate (CaCO3). It is a major component of limestone and marble.
Valentinite belongs to the antimony mineral group.
Talc belongs to the mineral group known as silicates.
Silicates are the mineral group that contain silicon, carbonates are the mineral group that contain carbon, halides are the mineral group that contain halogen elements, and sulfides are the mineral group that contain sulfur. Each of these mineral groups encompasses a variety of minerals with different chemical compositions.
Orothoclase Feldspar belong to the silicates group.
One example of a mineral that contains the CO3 group is calcite. Calcite is a common mineral that is composed of calcium carbonate (CaCO3). It is a major component of limestone and marble.
Bromide is not a major mineral group; it refers to a class of minerals containing the bromide ion (Br⁻). The major mineral groups typically include oxides, sulfates, and carbonates. Oxides are minerals containing oxygen and one or more metals, sulfates contain sulfate ions (SO₄²⁻), and carbonates contain carbonate ions (CO₃²⁻).
Zinc is a metal element and is not classified under a specific mineral group. It is commonly found in nature as the mineral sphalerite, which is a zinc sulfide.
The tourmaline group (cyclosilicates)
Chalcopyrite is in the sulfide mineral group.
Valentinite belongs to the antimony mineral group.
Ruby belongs to the mineral group Corundum
It is part of the sulphide mineral group.
Tremolite is a member of the amphibole mineral group.
Petroleum is the major mineral export.
Talc belongs to the mineral group known as silicates.
Silicates are the mineral group that contain silicon, carbonates are the mineral group that contain carbon, halides are the mineral group that contain halogen elements, and sulfides are the mineral group that contain sulfur. Each of these mineral groups encompasses a variety of minerals with different chemical compositions.