yes
Marble is metamorphosed limestone or dolomite. Primary composition is calcium carbonate. Veining is from non-calcitic impurities.
Sedimentary rocks are usually divided into: siliciclastic rocks and carbonate rocks. Siliciclastics are usually composed of the weathering products of older rocks carried and delivered to a basin of deposition by rivers. Carbonate rock, however, are generally composed of carbonate minerals (e.g. Calcite, Dolomite, Anhydrite..) these minerals form either biologically (as skeletons of sea organisms such as foraminifera, rudists and corals) or chemically by sea water. The most famous carbonate rock is probably Limestone, other rocks include: Dolostone (aka Dolomite) and evaporites; interesting to note that Marble is metamorphosed limestone.
Marble is metamorphosed limestone.
Marble is one form of metamorphosed limestone.
Limestone is the parent rock of marble. The word marble can be used to refer to both metamorphosed and unmetamorphosed limestone.
Marble is metamorphosed limestone or dolomite, and is predominately calcitic in composition. Marble usually forms from regional metamorphism associated with plate collisions.
Marble is metamorphosed limestone.
Marble is metamorphosed limestone or dolomite. Primary composition is calcium carbonate. Veining is from non-calcitic impurities.
Marble is metamorphosed limestone or dolostone.
Marble is the metamorphic rock formed from limestone. =)
No. Marble is metamorphosed limestone, recrystallized from heat, pressure, or both.
Yes, marble is metamorphosed limestone.
Marble is formed when limestone is metamorphosed. This process occurs when the mineral calcite in limestone recrystallizes due to heat and pressure, resulting in a denser, harder rock with a crystalline structure.
Marble (metamorphosed limestone) Slate (metamorphosed shale) Gneiss (metamorphosed granite)
Limestone - sedimentary deposition of calcarious marine organisms. Marble - compressed (metamorphosed) limestone.
Sedimentary rocks are usually divided into: siliciclastic rocks and carbonate rocks. Siliciclastics are usually composed of the weathering products of older rocks carried and delivered to a basin of deposition by rivers. Carbonate rock, however, are generally composed of carbonate minerals (e.g. Calcite, Dolomite, Anhydrite..) these minerals form either biologically (as skeletons of sea organisms such as foraminifera, rudists and corals) or chemically by sea water. The most famous carbonate rock is probably Limestone, other rocks include: Dolostone (aka Dolomite) and evaporites; interesting to note that Marble is metamorphosed limestone.
Marble is metamorphosed limestone.