Nd isotope composition of marine sediments as a tracer for iceberg provenance in the last glaciation

OMEX core KC 024-19 was studied aiming at to assess the influence of climate changes on the origin and transport of the sediments of the Galician continental slope, in the last 40 thousand years. The sampled sediments are composed mostly of silt and clay, but also include a coarser-grained (sand-siz...

ver descrição completa

Detalhes bibliográficos
Autor principal: Martins, V. (author)
Outros Autores: Santos, J. F. (author), Ribeiro, S. (author), Rocha, F. (author), Mackensen, A. (author), Rey, D. (author), Rubio, B. (author), Dias, J. M. A. (author)
Formato: article
Idioma:eng
Publicado em: 2013
Assuntos:
Galician continental slope
Heinrich events
Ice-rafted debris
Nd isotopes
Sediment provenance
Laurentide Ice Sheet
Texto completo:http://hdl.handle.net/10773/10619
País:Portugal
Oai:oai:ria.ua.pt:10773/10619

Texto Completo

http://hdl.handle.net/10773/10619

Registos relacionados