A sedimentary rock composed of calcium magnesium carbonate is known as dolomite. It forms from the mineral dolomite, which is similar to limestone but contains magnesium in addition to calcium. Dolomite often forms in marine environments through the replacement of limestone by magnesium-rich fluids.
Dolostone is primarily composed of the mineral dolomite, which is a carbonate mineral that contains magnesium. It also typically contains small amounts of other minerals like calcite, quartz, and clay minerals.
Yes, both limestone and chalk are forms of calcium carbonate. Limestone is a sedimentary rock composed mainly of calcium carbonate, while chalk is a soft, white, porous form of limestone composed of fossilized marine organisms.
Calcium carbonate makes limestone, while magnesium carbonate makes dolomite.
The sedimentary rock that forms calcium carbonate and fizzes in acid is likely limestone. Limestone is a common sedimentary rock primarily composed of calcite, a form of calcium carbonate. When exposed to acids such as vinegar or hydrochloric acid, limestone will fizz or effervesce due to the release of carbon dioxide gas.
Dolomite is a mineral consisting of calcium magnesium carbonate, while dolostone is a sedimentary rock primarily composed of the mineral dolomite. Dolostone forms when magnesium in seawater replaces some of the calcium in limestone during the rock's formation process.
Dolomite is not an ore itself; it is a mineral composed of calcium carbonate and magnesium carbonate. However, the main source of magnesium is magnesite, while the main source of calcium is limestone. Dolomite can be found in sedimentary rocks as a secondary mineral.
A dolomite deposit is a type of sedimentary rock containing the mineral dolomite, which is composed of calcium magnesium carbonate. These deposits typically form in ancient seabeds where magnesium-rich waters react with calcium carbonate-rich sediments. Dolomite deposits are commonly used in construction materials and agriculture due to their high magnesium content.
A sedimentary rock composed mainly of calcium carbonate.
Limestone is a sedimentary rock that is primarily composed of calcium carbonate, which is a form of carbon.
Fluorite is not a carbonate mineral. It is a halide mineral composed of calcium and fluorine (CaF2). Carbonate minerals, like calcite and dolomite, are composed of carbon, oxygen, and other elements like calcium or magnesium.
Limestone is a sedimentary rock primarily composed of calcium carbonate. Usually the remains of sea creatures are the original source of the calcium carbonate.
A calciturbidite is a turbidite - a sedimentary deposit formed by a turbidity current - composed of calcium carbonate.
Magnesium metal is extracted from dolomite, which is a mineral composed of calcium magnesium carbonate. The process typically involves thermal reduction of dolomite to produce magnesium metal and calcium oxide.
Dolostone is primarily composed of the mineral dolomite, which is a carbonate mineral that contains magnesium. It also typically contains small amounts of other minerals like calcite, quartz, and clay minerals.
Yes, both calcite and dolomite are carbonate minerals. Calcite is primarily composed of calcium carbonate (CaCO3), while dolomite is a carbonate mineral that contains calcium magnesium carbonate (CaMg(CO3)2).
Yes, both limestone and chalk are forms of calcium carbonate. Limestone is a sedimentary rock composed mainly of calcium carbonate, while chalk is a soft, white, porous form of limestone composed of fossilized marine organisms.
Calcium carbonate makes limestone, while magnesium carbonate makes dolomite.