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Questions related from Abhayanand Singh Maurya
To see the diagenetic environment or recrystallisation path whether the alteration of carbonate occurred in a open system or close system, how to plot d18O VPDB in D47 vs d18O VSMOW space
05 December 2017 1,408 0 View
The D47 temperature of top samples (off course weathered) from middle Eocene carbonates of Kutch, indicating lower temperature of 270C while corresponding benthic foraminifera temperature is...
13 September 2017 8,646 1 View
