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Mössbauer spectrometry to study diagenetical processes of red beds and sand dikes in the Valles-Penedes half graben

Author
Casas, Ll.; Parcerisa, D.; Gómez, D.; Calvet, F.; Roig, A.; Molins, E.
Type of activity
Presentation of work at congresses
Name of edition
International Conference on the Applications of the Mössbauer Effect 2001
Date of publication
2001
Presentation's date
2001-09
Book of congress proceedings
Hyperfine interactions (C): proceedings of the International Conference on the Applications of the Mössbauer Effect
First page
393
Last page
396
DOI
https://doi.org/10.1007/978-94-010-0281-3_97 Open in new window
URL
https://link.springer.com/chapter/10.1007/978-94-010-0281-3_97 Open in new window
Abstract
The Vallès-Penedès neogene half-graben (NE of Spain) is filled with a thick succession of terrigenous rocks, the lowermost unit of the basin consists of red-coloured clays, sandstones and conglomerates (red beds) formed in an alluvial fan environment. In the upper part of this unit some vertical joints are filled with blue sand (sand dikes). Sand dikes are interpreted as having been formed in an early stage after sedimentation. Despite the colour difference, the common sediment source of both,...
Keywords
Colour difference, Half graben, Mossbauer spectrometry, Mossbauer spectrum, Terrigenous rock
Group of research
ERNMA - Engineering of the Natural Resources and Environment
SSR-UPC - Smart Sustainable Resources

Participants

  • Casas, Lluís  (author and speaker )
  • Parcerisa Duocastella, David  (author and speaker )
  • Gómez Gras, David Manuel  (author and speaker )
  • Calvet Rovira, Francesc  (author and speaker )
  • Roig, Anna  (author and speaker )
  • Molins, E  (author and speaker )