This absence is reflected in numerous proxies, particularly the record of mass -
independent fractionation of sulfur isotopes.
The photochemical reaction of volcanic sulfur dioxide may not be the only method of creating a mass
independent fractionation of sulfur.
But rocks dating before 2.4 billion years ago have abnormal ratios, or exhibit mass
independent fractionation.
The occurrence of mass -
independent fractionation in the reaction of CO with OH raises fundamental questions about kinetic processes.
Not exact matches
Mass -
Independent Oxygen Isotope
Fractionation in Atmospheric CO as a Result of the Reaction CO + OH