Articles | Volume 17, issue 3
https://doi.org/10.5194/essd-17-1275-2025
https://doi.org/10.5194/essd-17-1275-2025
Data description paper
 | 
31 Mar 2025
Data description paper |  | 31 Mar 2025

SedDARE-IB: an open-access repository of sediment data for the Iberian Peninsula and its continental margins

Montserrat Torne, Tiago M. Alves, Ivone Jiménez-Munt, Joao Carvalho, Conxi Ayala, Elsa C. Ramalho, Angela María Gómez-García, Hugo Matias, Hanneke Heida, Abraham Balaguera, José Luis García-Lobón, and Jaume Vergés

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Cited articles

Alonso-Zarza, A. M., Clavo, J. P., Silva, P. G., and Torres, T.: Cuenca del Tajo, in: Geología de España, edited by: Vera, J. A., SGE-IGME, 556–561, ISBN 84-7840-546-1, 2004. 
Alves, T. M.: Networks of geometrically coherent faults accommodate Alpine tectonic inversion offshore southwestern Iberia, Solid Earth, 15, 39–62, https://doi.org/10.5194/se-15-39-2024, 2024. 
Alves, T. M. and Cunha, T. A.:. A phase of transient subsidence, sediment bypass and deposition of regressive–transgressive cycles during the breakup of Iberia and Newfoundland, Earth Planet. Sc. Lett., 484, 168–183, https://doi.org/10.1016/j.epsl.2017.11.054, 2018. 
Alves, T. M., Gawthorpe, R. L., Hunt, D. W., and Monteiro, J. H.: Cenozoic tectono-sedimentary evolution of the western Iberian margin, Mar. Geol., 195, 75–108, 2003a. 
Alves, T. M., Manuppella, G., Gawthorpe, R. L., Hunt, D. H., and Monteiro, J. H.: The depositional evolution of diapir- and fault-bounded rift basins: Examples from the Lusitanian Basin of west Iberia, Sediment. Geol., 162, 273–303, https://doi/10.1016/S0037-0738(03)00155-6, 2003b. 
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Short summary
Sediments are like history books for geologists and geophysicists. By studying them, we can learn about past environments, sea level and climate changes, and where the sediments came from. To aid in understanding the geology, georesources, and potential hazards in the Iberian Peninsula and its surrounding seas, we present the SedDARE-IB sediment data repository. As an application in geothermal exploration, we investigate how sediment thickness affects the depth of the 150 °C isotherm. 
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