Marble
is a metamorphic rock resulting from regional or, rarely, contact metamorphism
of sedimentary carbonate rocks (either limestone or dolomite rock) or
metamorphism of older. This metamorphic process causes a complete
recrystallization of the original rock into an interlocking mosaic of calcite,
aragonite and/or dolomite crystals.
The temperatures and pressures necessary to
form marble usually destroy any fossils and sedimentary textures present in the
original rock.
Pure
white marble is the result of metamorphism of very pure limestones. The
characteristic swirls and veins of many colored varieties are usually due to
various mineral impurities such as clay, silt, sand, iron oxides, or chert
which were originally present as grains or layers in the limestone. Green
coloration is often due to serpentine resulting from originally high magnesium
limestone or dolostone with silica impurities. These various impurities have
been mobilized and recrystallized by the intense pressure and heat of the
metamorphism.
Ground calcium carbonate is used in consumer products such as a food additive, in toothpaste, and as an inert filler in pills. It is used in plastics because it imparts stiffness, impact strength, dimensional stability, and thermal conductivity. It is used in paints because it is a good filler and extender, has high brightness, and is weather resistant. However, the growth in demand for ground calcium carbonate in the last decade has mostly been for a coating pigment in paper.
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