Controls on δ 34 S and δ 18 O of dissolved sulfate in aquifers of the Murray Basin, Australia and their use as indicators of flow processes

Author:

Dogramaci S.S,Herczeg A.L,Schiff S.L,Bone Y

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference42 articles.

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2. Geochemistry and isotope systematic of sulfur in the mixing zone of Bahamian blue holes;Bottrell;Appl. Geochem.,1991

3. Structural and stratigraphic framework of groundwater occurrence and surface discharge in the Murray Group Basin, southeastern Australia;Brown;BMR J. Austral Geol. Geophys,1989

4. Sulfur and oxygen isotopes of sulfate in precipitation and lake water, Quebec, Canada;Caron;Appl. Geochem.,1986

5. Isotopic constraints on the origin of salts in Australian Playas;Chivas;1. Sulfur. Palaegeogr., Palaeclimatol., Palaeoecol,1991

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