They consist of polygonal mosaic of predominantly homeoblastic fine grained calcite grains with isotropic fabric.
Polygonal mosaic marble geology.
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.
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It is composed primarily of the mineral calcite caco 3 and usually contains other minerals such as clay minerals micas quartz pyrite iron oxides and graphite under the conditions of metamorphism the calcite in the limestone recrystallizes to form a rock that is.
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The formation of granoblastic textures occurs to minimise the combined surface energy of phases within a rock.
Granoblastic polygonal texture a granoblastic texture is an equigranular texture in which crystals adopt a polygonal morphology with grain triple junctions of approximately 120 degrees.
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Instead only 7 of grains are 0 4 mm fig.
Mgs and mfs are 0 8 mm and 0 1 and 0 3 mm respectively in 68 of grains fig.
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The slightly rounded edges and the random wear areas of the forum finish evoque memories of the floors of the old european palaces.
Petrographic and cl characteristics are very similar to those described for the göktepe quarry.
Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism.