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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Language: | en |
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PERGAMON-ELSEVIER SCIENCE LTD
2016
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Online Access: | http://hdl.handle.net/10150/621924 http://arizona.openrepository.com/arizona/handle/10150/621924 |