Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard)
<p>The identification of sediment sources to the ocean is a pre-requisite to using ocean sediment cores to extract information on past climate and ocean circulation. Sr and Nd isotopes are classical tools with which to trace source provenance. Yet, despite considerable interest in the Arctic O...
Hoofdauteurs: | Hindshaw, R, Tosca, N, Piotrowski, A, Tipper, E |
---|---|
Formaat: | Journal article |
Gepubliceerd in: |
Copernicus Publications
2018
|
Gelijkaardige items
-
Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard)
door: R. S. Hindshaw, et al.
Gepubliceerd in: (2018-03-01) -
Experimental constraints on Mg isotope fractionation during clay formation: implications for the global biogeochemical cycle of Mg
door: Hindshaw, RS, et al.
Gepubliceerd in: (2019) -
Experimental constraints on Li isotope fractionation during clay formation
door: Hindshaw, R, et al.
Gepubliceerd in: (2019) -
Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments
door: Ruth S. Hindshaw, et al.
Gepubliceerd in: (2018-07-01) -
The distribution of neodymium isotopes in Arctic Ocean basins
door: Porcelli, D, et al.
Gepubliceerd in: (2009)