HIGHLIGHTS
SUMMARY
The characteristics of dolomitic marbles have been described since 1791 by the Commander Déodat de Dolomieu, a French geologist, in a letter addressed to Mr. Picot de La Peyrouse and published in the Journal de Physique. Since that time, the two varieties of white marbles, dolomitic and calcitic, have been studied and can be distinguished by their chemical composition: calcite is a crystalized calcium carbonate, whereas dolomite is a crystalized calcium magnesium carbonate. 13C NMR spectra of all of the samples were recorded with a 9.4 T Avance NMR apparatus from Bruker . . .
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