== Limestone, dolomite and marble are carbonate rocks.
Metamorphosed limestone or dolomite. Calcium, Carbon, Oxygen, Magnesium (dolomitic marble only).
Marble is metamorphosed limestone or dolomite. Primary composition is calcium carbonate. Veining is from non-calcitic impurities.
Calcite
There are several mineral deposits in the island country of the Philippines. The country has shown much potential for copper, gold, nickel, chromite, and other metals, as well as marble, limestone, clays, feldspar, rock aggregates, and dolomite.
The parent rock of marble can be composed of calcite or dolomite. Thus, it can be one of several rock types, often limestone (though it can conceivably also be dolomite or travertine, etc.). Limestone is considered to be the most common parent rock of marble. Since it is composed of calcite, it can be tested with dilute hydrochloric acid. If it bubbles, it is composed of calcite, and is probably marble.
Marble is a metamorphic rock. It is a metamorphism of limestone or dolostone and contains calcite and dolomite.
The metamorphosed form of dolomite is called marble. Dolomite is a sedimentary rock primarily composed of the mineral dolomite, while marble is a metamorphic rock that forms from the recrystallization of limestone or dolomite under high heat and pressure.
Marble is metamorphosed limestone or dolomite, and is predominately calcitic in composition. Marble usually forms from regional metamorphism associated with plate collisions.
Marble is a metamorphic rock. It is a metamorphism of limestone or dolostone and contains calcite and dolomite.
calcite and dolomite.
Marble is mainly composed of CaCO3 (calcium carbonate, limestone) in which calcium is the metallic ion.
Marble is in the carbonate mineral group. Limestone and dolomite are also in the carbonate mineral group. Marble is formed from limestone.
The protolith of marble was limestone or dolomite.
The protolith of marble was limestone or dolomite.
A metamorphic form of limestone is marble.
marble
A conglomerate and a limestone both are sedimentary rocks.