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Questions related from Himadri Basu
Analysis of a carbonate (calcite vein) sample yielded d18O of 6.09 (V-SMOW) and d13C of -4.23 (V-PDB), and only 47 ppm Sr. Stable isotopic data indicate 'mantle signature', while Sr abundance is...
06 October 2021 2,039 6 View
CO2 is normally isotopically depleted compared to carbonate rocks (e.g. limestone). However, CO2 liberated during decarbonation of carbonate rocks are enriched in both O18 and C13. Why?
08 June 2021 1,922 4 View
Pyrites are known to form in low-temperature sedimentary to high-temperature magmatic environments. They also form from extensively wide variety of ore-bearing fluids. S isotope data often helps...
12 May 2021 6,144 4 View
For normalizing REE data of fine siliciclastic rocks both PAAS as well as Chondrite values are used. Ideally both would given similar normalized REE pattern. Please suggest me which normalization...
02 July 2016 7,691 11 View
In a ferruginous sandstone sample I found very well rounded quartz grains are floating in ferruginous matrix and cement. I suspect it to be floating texture. I want more detailed information on it.
22 November 2013 6,525 3 View