The mineral dolomite is commonly found in deposits of a sedimentary rock called dolostone. Dolomite limestone, which is just an irregular mixture of calcium and magnesium carbonates. Dolomite is believed to have formed by replacement of some of the calcium in a calcium carbonate limestone deposit with magnesium. The calcium and magnesium ions in dolomite exist.
Dolomite has a calcium layer, then a carbonate layer, then a magnesium layer then a carbonate layer, and so on. Dolomite is available in different particle size ranges: 100#, 200#, 250#, 300#, 400#, 500#, also available as per customer’s specification. Dolomite is harder and denser than the calcite form of calcium carbonate or limestone.
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|Size :||As Per Requirement|