Estudio paleomagnético preliminar de una sucesión lacustre pliocena en la Depresión de la Selva(cordilleras Costero Catalanas, NE península Ibérica)

  1. Á. Carrancho 1
  2. J.J Villalaín 1
  3. B. Gómez de Soler 2
  4. G. Campeny 2
  5. O. Oms 3
  6. J. Agustí 2
  7. J. van der Made 4
  8. H-A. Blain 2
  9. F. Burjachs 2
  10. G. Jiménez-Moreno 5
  11. I. Expósito 2
  12. E. Barrón 6
  1. 1 Universidad de Burgos
    info

    Universidad de Burgos

    Burgos, España

    ROR https://ror.org/049da5t36

  2. 2 Universitat Rovira i Virgili
    info

    Universitat Rovira i Virgili

    Tarragona, España

    ROR https://ror.org/00g5sqv46

  3. 3 Universitat Autònoma de Barcelona
    info

    Universitat Autònoma de Barcelona

    Barcelona, España

    ROR https://ror.org/052g8jq94

  4. 4 Museo Nacional de Ciencias Naturales
    info

    Museo Nacional de Ciencias Naturales

    Madrid, España

    ROR https://ror.org/02v6zg374

  5. 5 Universidad de Granada
    info

    Universidad de Granada

    Granada, España

    ROR https://ror.org/04njjy449

  6. 6 Instituto Geológico y Minero de España (IGME)
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Journal:
Geotemas (Madrid)

ISSN: 1576-5172

Year of publication: 2012

Issue Title: VIII Congreso Geológico de España, Oviedo, 17-19 de julio, 2012.

Issue: 13

Pages: 1136-1139

Type: Article

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Abstract

Preliminary palaeomagnetic and rock-magnetic results obtained in two cores extracted from the lacustrine sequence that infills the Camp dels Ninots maar (Caldes de Malavella, Girona, NE Spain) are presented here. The particular sedimentary conditions of the site have allowed an excellent preservation of the spectacular Pliocene fossils recovered. These are represented by macro and microvertebrates –generally in anatomical connection-, including rodents, turtles, amphibians and fishes, among others remains. This palaeoentological record suggest a Pliocene age for the site (3.5 – 3.2 M.a.). Several magnetozones of different polarities but similar magnetic properties (coexisting magnetite and greigite) have been identified which we preliminarily attribute to the record of Kaena and/or Mamooth subchrons within the Gauss normal polarity Chron.

Data source: Dialnet