Carbon and oxygen isotope geochemistry of Neoproterozoic limestones of the Shahabad Formation, Bhima basin, Karnataka, southern India
PDF

Keywords

geochemistry
stable isotopes
delta oxygen
delta carbon
strontium isotopes
carbonate rocks
diagenesis
Bhima basin
India.

How to Cite

Nagarajan, R., Sial, A. N., Armstrong-Altrin, J. S., Madhavaraju, J., & Nagendra, R. (2018). Carbon and oxygen isotope geochemistry of Neoproterozoic limestones of the Shahabad Formation, Bhima basin, Karnataka, southern India. Revista Mexicana De Ciencias Geológicas, 25(2), 225–235. Retrieved from https://rmcg.unam.mx/index.php/rmcg/article/view/654

Citas en Dimensions Service

Share on

Abstract

Petrography, major (including four trace elements), stable isotopes (carbon and oxygen), and 87Sr/86Sr geochemistry of limestones of the Shahabad Formation, Bhima basin, Karnataka, southern India are reported. These limestones show a narrow range of δ13C (~1.34−1.96‰) and δ18O (~ -6.04 to -7.61‰) values. The petrographic study reveals the presence of microsparite and micro- and macrostylolites. The δ13C and 87Sr/86Sr values indicate that these limestones were deposited during the late Neoproterozoic age and the δ18O values also are very similar to the average Proterozoic carbonate values. Mn and Sr concentrations and low Mn/Sr ratio (<1) together with the stable and radiogenic isotope data suggest that the studied samples are well-preserved or scarcely altered limestones and probably have retained their primary isotopic signatures.

 


 

PDF

Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 International License.

Downloads

Download data is not yet available.