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-...

Full description

Bibliographic Details
Main Author: Martins, V. (author)
Other Authors: 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)
Format: article
Language:eng
Published: 1000
Subjects:
Paleoclimate
Heinrich Events
Ice rafted debris provenance
Sr and Nd isotopes
Online Access:http://hdl.handle.net/10773/11601
Country:Portugal
Oai:oai:ria.ua.pt:10773/11601

Internet

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

Similar Items