Geochemical and C-O isotopic study of ophiolite-derived carbonates of the Barzaman Formation, Oman: Evidence of natural CO2 sequestration via carbonation of ultramafic clasts

Major, trace, and REE data obtained by ICP-OES and ICP-MS techniques for carbonate rocks from the Barzaman Formation in Oman. C-O isotope data obtained by IRMS technique are also included for a model to determine the amount of CO2 stored by a carbonate sample precipitated via alteration of the Oman Ophiolite.