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...
Главные авторы: | Hindshaw, R, Tosca, N, Piotrowski, A, Tipper, E |
---|---|
Формат: | Journal article |
Опубликовано: |
Copernicus Publications
2018
|
Схожие документы
-
Clay mineralogy, strontium and neodymium isotope ratios in the sediments of two High Arctic catchments (Svalbard)
по: R. S. Hindshaw, и др.
Опубликовано: (2018-03-01) -
Experimental constraints on Mg isotope fractionation during clay formation: implications for the global biogeochemical cycle of Mg
по: Hindshaw, RS, и др.
Опубликовано: (2019) -
Experimental constraints on Li isotope fractionation during clay formation
по: Hindshaw, R, и др.
Опубликовано: (2019) -
Li and U Isotopes as a Potential Tool for Monitoring Active Layer Deepening in Permafrost Dominated Catchments
по: Ruth S. Hindshaw, и др.
Опубликовано: (2018-07-01) -
The distribution of neodymium isotopes in Arctic Ocean basins
по: Porcelli, D, и др.
Опубликовано: (2009)