Eventos de Heinrich reconocidos mediante parámetros magneto-mineralógicos en sedimentos del Pleistoceno Superior del margen gallego

  1. R. Coimbra 1
  2. D. Rey 1
  3. K. Mohamed 1
  4. P. Álvarez-Iglesias 1
  5. F. Vilas 1
  6. T. Frederichs 2
  1. 1 Universidade de Vigo
    info

    Universidade de Vigo

    Vigo, España

    ROR https://ror.org/05rdf8595

  2. 2 University of Bremen
    info

    University of Bremen

    Brema, Alemania

    ROR https://ror.org/04ers2y35

Libro:
Contribuciones al estudio del periodo cuaternario
  1. Lario Gómez, Javier (coord.)
  2. Silva, Pablo G. (coord.)

Editorial: Escuela Técnica Superior de Ingenieros Industriales de Madrid ; Universidad Politécnica de Madrid

ISBN: 978-84-7484-201-2

Año de publicación: 2007

Páginas: 183-184

Tipo: Capítulo de Libro

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Resumen

Three gravity cores extracted from the Galicia margin were studied in order to identify and characterize Heinrich layers. Magnetic parameters such as magnetic susceptibility (κ), ARM100 and low temperature measurements (remanence and susceptibility) were used to determine the mineralogical components of these events. The development of loops on the ARM100 vs. K plot shows an increasing grain size trend at these levels. This feature, along with the identification of stoicheometricmagnetite grains by low temperature techniques, supports that ice rafting was responsible for the transport of such material to the Galician margin.

Fuente de los datos: Dialnet