Oxygen and carbon isotope fractionation between dolomite and calcite in lesser Himalayan and Vindhyan limestones

Details Oxygen and carbon isotope fractionation between dolomite and calcite in lesser Himalayan and Vindhyan limestones Oxygen and carbon isotope fractionation between dolomite and calcite in lesser Himalayan and Vindhyan limestones

May 1970

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1970gecoa..34..625p&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 34, Issue 5, pp.625-628

Physics

1

Scientific paper

X-ray analysis of limestones from the Lesser Himalyan and Vindhyan systems showed the presence of calcite and dolomite. The O 18 / O 16 and C 13 / C 12 ratios of the calcite and dolomite fractions showed that dolomite is in general enriched in C 13 and depleted in O 18 contents with respect to calcite. The negative values of the oxygen isotope fractionation factor suggest that the two fractions were not formed under isotopic equilibrium conditions.

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