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 Universitat de Barcelona
    info
    Universitat de Barcelona

    Barcelona, España

    ROR https://ror.org/021018s57

    Geographic location of the organization Universitat de Barcelona
  2. 2 Instituto de Ciencias de la Tierra Jaume Almera
    info
    Instituto de Ciencias de la Tierra Jaume Almera

    Barcelona, España

    ROR https://ror.org/01nsd7y51

    Geographic location of the organization Instituto de Ciencias de la Tierra Jaume Almera
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.