Caracterización de los sedimentos superficiales en tres sistemas deposicionales contorníticos (Golfo de Cádiz, Cabo Ortegal y El Cachucho)implicaciones conceptuales

  1. I. Alejo 1
  2. M.A. Nombela 1
  3. G. Ercilla 2
  4. R.E. Brackenridge 3
  5. G. Francés 1
  6. M. Pérez-Arlucea 1
  7. A. Mena 1
  8. F.J. Hernández-Molina 1
  9. D.A.V. Stow 3
  10. T. Medialdea 4
  1. 1 Universidade de Vigo
    info

    Universidade de Vigo

    Vigo, España

    ROR https://ror.org/05rdf8595

  2. 2 CSIC, Instituto Ciencias del Mar
  3. 3 ECOSSE, Heriot-Watt University, Edinburgh
  4. 4 Instituto Geológico y Minero de España
    info

    Instituto Geológico y Minero de España

    Madrid, España

    ROR https://ror.org/04cadha73

Revista:
Geotemas (Madrid)

ISSN: 1576-5172

Ano de publicación: 2012

Título do exemplar: VIII Congreso Geológico de España, Oviedo, 17-19 de julio, 2012.

Número: 13

Páxinas: 1781-1784

Tipo: Artigo

Outras publicacións en: Geotemas (Madrid)

Resumo

Compositional, mineralogical and grain size data from 13 superficial samples recovered between 490 and 1144 m water depth in three Contourite Depositional Systems (CDSs): the Gulf of Cadiz, Ortegal Spur and El Cachucho are presented. First surficial centimeter was analysed in different contourite features: depositional (drifts), erosive (moats) and mixed (terraces). Analysed sediments show a broad variability in grain size, from bioclastic gravels to azoic fine silts. There is no clear particle size difference between the three studied CDSs, but there is a similar textural trend between the contourite features and the textural pattern. Coarser samples are located both in moats and terraces, with medium (300 µm in the El Cachucho) and coarse sands (600 µm in Gulf of Cadiz and Ortegal Spur). Many samples have foraminifers and glauconite in different percentages. The most abundant minerals in all samples are quartz (34.7-77.8%) and calcite (14.1-42.9%). Magnesium calcite (1-15.8%) appears in all samples,, and albite (1-5%) and microcline (2- 5%) occur in most of them Surface sediment characterization and classification is essential for contourite facies estimation, not well established yet.