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...
Κύριοι συγγραφείς: | Hindshaw, R, Tosca, N, Piotrowski, A, Tipper, E |
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Μορφή: | Journal article |
Έκδοση: |
Copernicus Publications
2018
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Παρόμοια τεκμήρια
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Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard)
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Experimental constraints on Mg isotope fractionation during clay formation: implications for the global biogeochemical cycle of Mg
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Experimental constraints on Li isotope fractionation during clay formation
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Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments
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The distribution of neodymium isotopes in Arctic Ocean basins
ανά: Porcelli, D, κ.ά.
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