Analizando la cinética de las remagnetizaciones por enterramientoel caso de la Cuenca turbidítica de Jaca (Pirineos occidentales)

  1. P. Calvín 1
  2. E.L. Pueyo 1
  3. J.C. Larrasoaña 1
  4. R. Egli 2
  5. A. Rodríguez-Pintó
  6. E. Izquierdo-Llavall 3
  7. B. Oliva-Urcia 4
  8. E. Beamud 5
  9. A. Payros 6
  10. M.P. Mata 1
  11. A. Orera 7
  12. E. Bellido 1
  13. A. Luzón 7
  14. I. Gil-Peña 1
  15. G. Bernaola 6
  16. M. Montes 1
  17. J.M. Samsó
  18. R. Toro 7
  1. 1 Instituto Geológico y Minero de España
    info

    Instituto Geológico y Minero de España

    Madrid, España

    ROR https://ror.org/04cadha73

  2. 2 Central Institution for Meteorology and Geodynamics
    info

    Central Institution for Meteorology and Geodynamics

    Viena, Austria

    ROR https://ror.org/048dqgk17

  3. 3 University of Pau and Pays de l'Adour
    info

    University of Pau and Pays de l'Adour

    Pau, Francia

    ROR https://ror.org/01frn9647

  4. 4 Universidad Autónoma de Madrid
    info

    Universidad Autónoma de Madrid

    Madrid, España

    ROR https://ror.org/01cby8j38

  5. 5 Consejo Superior de Investigaciones Científicas
    info

    Consejo Superior de Investigaciones Científicas

    Madrid, España

    ROR https://ror.org/02gfc7t72

  6. 6 Universidad del País Vasco/Euskal Herriko Unibertsitatea
    info

    Universidad del País Vasco/Euskal Herriko Unibertsitatea

    Lejona, España

    ROR https://ror.org/000xsnr85

  7. 7 Universidad de Zaragoza
    info

    Universidad de Zaragoza

    Zaragoza, España

    ROR https://ror.org/012a91z28

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Zeitschrift:
Geotemas (Madrid)

ISSN: 1576-5172

Datum der Publikation: 2021

Titel der Ausgabe: X Congreso Geológico de España

Nummer: 18

Seiten: 709

Art: Artikel

DIALNET GOOGLE SCHOLAR lock_openOpen Access editor

Andere Publikationen in: Geotemas (Madrid)

Zusammenfassung

Burial related chemical remagnetizations are a common process in sedimentary basins and orogenic wedges worldwide. It involves authigenic formation of ferromagnetic minerals s.l. related with enhanced temperature conditions during burial. However, the kinetic of these processes remains unsolved partially because most of the best-documented cases occurred during magnetic superchrons. The sedimentary sequence of the Eocene Jaca turbiditic Basin (Western Pyrenees) displays a dual polarity record of a burial remagnetization that records different chrons along the sedimentary sequence. This outstan- ding case study offers the possibility to carry out a multidisciplinary study relating temperature, magnetic mineralogy and remagnetization time in the frame of the UKRIA4D project (PID2019-104693GB-I00/CTA).

Fuente de los datos: Dialnet