Stable chlorine isotopes in arid non-marine basins: Instances and possible fractionation mechanisms

Stable chlorine isotopes are useful geochemical tracers in processes involving the formation and evolution of evaporitic halite. Halite and dissolved chloride in groundwater that has interacted with halite in arid non-marine basins has a delta Cl-37 range of 0 +/- 3 parts per thousand, far greater t...

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Bibliographic Details
Main Author: Eastoe, C.J.
Other Authors: University of Arizona
Language:en
Published: PERGAMON-ELSEVIER SCIENCE LTD 2016
Subjects:
Online Access:http://hdl.handle.net/10150/621924
http://arizona.openrepository.com/arizona/handle/10150/621924