Marble is a metamorphic rock consisting of carbonate minerals that recrystallize under the influence of heat, pressure, and aqueous solutions. It is typically not foliated and has a crystalline texture of varying thickness. The rock is formed through the metamorphism
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Marble is a metamorphic rock composed of carbonate minerals that undergo recrystallization due to heat, pressure, and aqueous solutions, resulting in a crystalline texture of varying thickness. While typically not foliated, there are exceptions. The production of
Marble is a metamorphic rock that forms through the recrystallization of carbonate minerals under high heat, pressure, and aqueous solutions, commonly calcite or dolomite. It has a varying thickness and a crystalline texture. Unlike most metamorphic rocks, marble is