Determinación del polo paleomagnético para el límite Oligoceno-Mioceno en la Cuenca del Ebro

  1. X. Barbera 1
  2. L. Cabrera 1
  3. E. Gomis 2
  4. J.M. Parés 2
  1. 1 Grupo de Geodinámica y Análisis de Cuencas. Dep. Geologia Dinamica, Geofisica i Paleontologia. Universitat de Barcelona
  2. 2 Institut de Ciéncies de la Terra "Jaume Almera» (CSIC). Barcelona
Journal:
Geogaceta

ISSN: 0213-683X

Year of publication: 1996

Issue: 20

Pages: 1014-1016

Type: Article

More publications in: Geogaceta

Abstract

A paleomagnetic study was carried out in Oligocene-Miocene fluvial and lacustrine sediments of the Ebro Basin. A significative number of samples are treated. A Paleomagnetic Pole for the OligoceneMiocene boundary in the Ebro Basin has been obtained (Lat. = 79.6° N, Long. = 155.9° E, lX 9S= 5.9). This results indicate no significative rotations for the Ebro Basin since the upper Oligocene.