Dense and hypodense fascicles marble like pattern spindled cells with irregular nuclei. Marble is a metamorphic rock composed of recrystallized carbonate minerals most commonly calcite or dolomite marble is typically not foliated although there are exceptions in geology the term marble refers to metamorphosed limestone but its use in stonemasonry more broadly encompasses unmetamorphosed limestone. The alternation of sharply demarcated hypercellular and hypocellular zones gives rise to a marble appearance.
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