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Carbon and Oxygen Isotopic Study of Limestones from the Triassic Lower Krol Formation of India


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1 Jawaharlal University, New Delhi, India
 

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The O18/O16 and C13/C12 ratios of dolomite and calcite from Rajpur area on the Dehra Dun-Mussori road have been reported. The samples belong to the Lower Krol Formations of Triassic age. The isotopic composition data have been utilised to determine the conditions of formation. The data indicate that the precipitation occurred in warm waters and under isotopic equilibrium conditions.
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  • Carbon and Oxygen Isotopic Study of Limestones from the Triassic Lower Krol Formation of India

Abstract Views: 277  |  PDF Views: 117

Authors

G. C. Pandey
Jawaharlal University, New Delhi, India

Abstract


The O18/O16 and C13/C12 ratios of dolomite and calcite from Rajpur area on the Dehra Dun-Mussori road have been reported. The samples belong to the Lower Krol Formations of Triassic age. The isotopic composition data have been utilised to determine the conditions of formation. The data indicate that the precipitation occurred in warm waters and under isotopic equilibrium conditions.