Experimental constraints on Li isotope fractionation during clay formation
<br/>Knowledge of the lithium (Li) isotope fractionation factor during clay mineral formation is a key parameter for Earth system models. This study refines our understanding of isotope fractionation during clay formation with essential implications for the interpretation of field data and the...
Main Authors: | Hindshaw, R, Tosca, R, Gout, T, Farnan, I, Tosca, N, Tipper, E |
---|---|
Format: | Journal article |
Published: |
Elsevier
2019
|
Similar Items
-
Experimental constraints on Mg isotope fractionation during clay formation: implications for the global biogeochemical cycle of Mg
by: Hindshaw, RS, et al.
Published: (2019) -
Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard)
by: Hindshaw, R, et al.
Published: (2018) -
Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard)
by: R. S. Hindshaw, et al.
Published: (2018-03-01) -
Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments
by: Ruth S. Hindshaw, et al.
Published: (2018-07-01) -
Diagenetic pathways linked to labile Mg-clays in lacustrine carbonate reservoirs: a model for the origin of secondary porosity in the Cretaceous pre-salt Barra Velha Formation, offshore Brazil
by: Tosca, N, et al.
Published: (2015)