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

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...

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Bibliographische Detailangaben
Hauptverfasser: Ali, Arshad, Abbasi, Iftikhar Ahmed, Nogueira, Leonardo Brandão, Hersi, Osman Salad, Al Kindi, Sumaiya A. N., El-Ghali, Mohamed A.K., Nasir, Sobhi
Format: Dataset
Sprache:eng
Schlagworte:
Carbon Sequestration Science
FOS: Agriculture, forestry and fisheries
FOS: Earth and related environmental sciences
Geology
Inorganic Geochemistry
Isotope Geochemistry
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Zusammenfassung: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.
DOI:10.6084/m9.figshare.14723568