This book provides detailed information on the history, analysis
and applications of chlorine and bromine isotope geochemistry.
Chlorine and bromine are geochemically unique as they prefer to
exist as single charged negative ions. For this reason isotope
fractionation reflects mostly processes that are not related to
changes in the redox state and this fractionation is generally
modest. The book will describe the processes that are most easily
detected using these isotopes. Also isotope variations, and
processes that cause them, measured in oxidised species such as
perchlorates and in organic molecules will be described in this
book.
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