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...

Full description

Bibliographic Details
Main Author: Martins, V. (author)
Other Authors: Santos, J. F. (author), Ribeiro, S. (author), Rocha, F. (author), Mackensen, A. (author), Rey, D. (author), Rubio, B. (author), Dias, J. M. A. (author)
Format: article
Language:eng
Published: 2013
Subjects:
Galician continental slope
Heinrich events
Ice-rafted debris
Nd isotopes
Sediment provenance
Laurentide Ice Sheet
Online Access:http://hdl.handle.net/10773/10619
Country:Portugal
Oai:oai:ria.ua.pt:10773/10619

Internet

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

Similar Items