De la Cuenca Interior de Galicia (NW Iberia), las Masas de Hielo Noratlánticas y la procedencia de los IRD

  1. M. Plaza-Morlote 1
  2. D. Rey 1
  3. J.F. Santos 2
  4. S. Ribeiro 2
  5. D. Heslop 3
  6. A. Bernabéu 1
  7. K.J. Mohamed 1
  8. B. Rubio 1
  9. V. Martíns 4
  1. 1 Universidade de Vigo
    info

    Universidade de Vigo

    Vigo, España

    ROR https://ror.org/05rdf8595

  2. 2 Universidade de Aveiro
    info

    Universidade de Aveiro

    Aveiro, Portugal

    ROR https://ror.org/00nt41z93

  3. 3 Australian National University Canberra
  4. 4 Universidade do Estado do Rio de Janeiro
    info

    Universidade do Estado do Rio de Janeiro

    Río de Janeiro, Brasil

    ROR https://ror.org/0198v2949

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Journal:
Geotemas (Madrid)

ISSN: 1576-5172

Year of publication: 2016

Issue Title: IX CONGRESO GEOLÓGICO DE ESPAÑA

Issue: 16

Pages: 165-168

Type: Article

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More publications in: Geotemas (Madrid)

Abstract

In this study they are presented and discussed the results relating to the Ice Rafted Detritus (IRD) provenance of the last six Heinrich Events (HE) in the North West Iberian margin. The research is based on the Neodymium and Strontium isotopic fingerprint in the coarse detrital fraction of the sediment core CI12PC3, from the Galicia Interior Basin (NE Atlantic). This is the second work concerning to the IRD provenance in the NW Iberian Margin, after the findings made by Martins et al. (2013), and the first one to present provenance results for the last six HE in this margin.

Data source: Dialnet