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Volumn 333-334, Issue , 2012, Pages 35-45

Positive correlation between Li and Mg isotope ratios in the river waters of the Mackenzie Basin challenges the interpretation of apparent isotopic fractionation during weathering

Author keywords

Chemical weathering; Li isotopes; Lithium; Magnesium; Mg isotopes; River geochemistry

Indexed keywords

CATION EXCHANGES; CHEMICAL WEATHERING; CLAY CONTENT; COVARIATION; DATA SETS; ISOTOPIC COMPOSITION; ISOTOPIC FRACTIONATIONS; LARGE ION LITHOPHILE ELEMENTS; LI ISOTOPES; MG CONTENT; MG ISOTOPES; PHYSICOCHEMICAL PROCESS; POSITIVE CORRELATIONS; RIVER WATER; SEDIMENT CONCENTRATION; SILICATE ROCKS; SILICATE WEATHERING; SINGLE PROCESS; SOLUTE CONCENTRATIONS; STABLE ISOTOPE DATA; STABLE ISOTOPES; WATERBODIES;

EID: 84861172606     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2012.04.023     Document Type: Article
Times cited : (105)

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