The sources of the glacial IRD in the NW Iberian Continental Margin over the last 40 ka

In this work, the first results of ice rafted detritus (IRD) provenance related to Heinrich Events in the NW Iberian Margin are presented and discussed. This study is based on multiproxies but thoroughly analyzes Sr and Nd isotope ratios measured in the detrital fraction of the sediment core KC 024-...

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Detalhes bibliográficos
Autor principal: Martins, V. (author)
Outros Autores: Santos, J. F. (author), Mackensen, A. (author), Dias, J. M. A. (author), Ribeiro, S. (author), Moreno, J. (author), Soares, A. M. (author), Frontalini, F. (author), Rey, D. (author), Rocha, F. (author)
Formato: article
Idioma:eng
Publicado em: 1000
Assuntos:
Paleoclimate
Heinrich Events
Ice rafted debris provenance
Sr and Nd isotopes
Texto completo:http://hdl.handle.net/10773/11601
País:Portugal
Oai:oai:ria.ua.pt:10773/11601

Texto Completo

http://hdl.handle.net/10773/11601

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