Por favor, use este identificador para citar o enlazar a este item:
http://hdl.handle.net/10261/194540
COMPARTIR / EXPORTAR:
SHARE BASE | |
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE | |
Título: | Seismic Study of the Iberian Crust, ESCI-North survey |
Autor: | Pérez-Estaún, Andrés CSIC; Gallart Muset, Josep CSIC ORCID; Pulgar, J. A.; Alvarez-Marrón, Joaquina CSIC ORCID | Palabras clave: | Field Seismic:Active:MCS DigitalSeg SEGY Seismic:Reflection Seismometer_SingleFrequency Hydrophone_Streamer SeismicSource_Explosive SeismicSource_Gun_Air |
Fecha de publicación: | 13-nov-2019 | Editor: | DIGITAL.CSIC | Citación: | Pérez-Estaún, A., Gallart, J., Pulgar, J. A., Álvarez-Marrón, J.; [2019]; "Seismic Study of the Iberian Crust, ESCI-North survey. [Dataset]"; DIGITAL.CSIC; http://dx.doi.org/10.20350/digitalCSIC/9894 | Resumen: | The ESCI-N project in Northwestern Spain was a subprogram of the ESCI Program (Estudios Sísmicos de la Corteza Ibérica). It is formed by four seismic experiments both on and offshore. This project aimed to image the Cantabrian Zone, West Asturian-Leonese Zone and the northern Iberian margin, thus characterizing the crustal structure resulted from the Variscan and Alpine orogenies and the Mesozoic extension related to the opening of the Bay of Biscay. | Descripción: | Two onshore profiles were acquired in E-W and N-S directions through the Variscan and Alpine domains of 140 and 65 km length, ESCI-N1 and ESCI-N2 respectively. Also two offshore profiles ESCI-N3 and ESCI-N4 were obtained with a streamer of 4500 m having 360 channels with a 12.5 m gap between them and a 40 l airgun capacity. ESCI-N3 follows a swerved line in a mainly E-W direction crossing the Variscan structures. ESCI-N4 is a N-S direction profile that crosses both the Cantabrian margin and Le Danois bank Alpine structures. Techincal specifications of offshore profiles: streamer length 4,500 m, 360 channels, group interval 12,5 m and sample rate 4 ms. | URI: | http://hdl.handle.net/10261/194540 | DOI: | 10.20350/digitalCSIC/9894 | Referencias: | Teixell, A., Labaume, P., Ayarza, P., Espurt, N., de Saint Blanquat, M., and Lagabrielle, Y. (2018). Crustal structure and evolution of the Pyrenean-Cantabrian belt: A review and new interpretations from recent concepts and data. Tectonophysics 724-725, 146-170. https://doi.org/10.1016/j.tecto.2018.01.009 Gallastegui, J., Pulgar, J.A., and Gallart, J. (2016). Alpine tectonic wedging and crustal delamination in the Cantabrian Mountains (NW Spain). Solid Earth, 7, 1043–1057. http://dx.doi.org/10.5194/se-7-1043-2016 Díaz, J., Gallart, J., Pulgar, J.A., Ruiz, M., and Pedreira, P. (2009). Crustal structure beneath North-West Iberia imaged using receiver functions. Tectonophysics 478, 175-183. https://doi.org/10.1016/j.tecto.2009.08.003 Martínez Catalán, J.R., Ayarza, P., and Pulgar, J,.A. (2004). La estructura profunda de la zona asturoccidental-leonesa deducida del perfil sísmico ESCI-N3.3. Geología de España, 60-63 Fernández-Viejo, G., Gallart, J., Pulgar, J.A., Gallastegui, J., Dañobeitia, J.J., and Córdoba, D. (1998). Crustal transition between continental and oceanic domains along the North Iberian margin from wide angle seismic and gravity data. Geophysical Research Letters, vol. 25, no. 23, 4249-4252 p. http://dx.doi.org/10.1029/1998GL900149 Pérez-Estaún, A., Pulgar, J.A., Alvarez-Marron, J., and ESCI-N Research Group (1997). Crustal structure of the Cantabrian Zone: seismic image of a Variscan foreland thrust and fold belt (NW Spain). Revista de la Sociedad Geológica de España 8 (4), 1995: 307-319. http://www.sociedadgeologica.es/archivos/REV/8(4)/Art01.pdf Martínez Catalán, J.R., Ayarza Arribas, P., Pulgar, J.A., Pérez-Estaún, A., Gallart, J., Marcos, A., Bastida, F., Álvarez-Marrón, J., González-Lodeiro, F., Aller, J., Dañobeitia, J.J., Banda, E., Córdoba, D., and Comas, M.C. (1997). Results from the ESCI-N3.3 marine deep seismic profile along the Cantabrian continental margin. Revista de la Sociedad Geológica de España 8 (4), 1995: 341-354. http://hdl.handle.net/10261/171610 Gallart, J., Fernández- Viejo, G., Díaz, J., Vidal, N. and Pulgar, J.A. (1997). Deep structure of the transition between the Cantabrian Mountains and the North Iberian Margin from wide-angle ESCI-N data. Revista de la Sociedad Geológica de España 8 (4), 1995: 365- 382. http://www.sociedadgeologica.es/archivos/REV/8(4)/Art06.pdf Pulgar, J.A., Pérez-Estaún, A., Gallart, J., Álvarez-Marrón, J., Gallastegui, J., Alonso, J.L., and ESCIN Group (1997). The ESCI-N2 deep seismic reflection profile: a traverse across the Cantabrian Mountains and adjacent Duero basin. Revista de la Sociedad Geológica de España 8 (4), 1995: 383-394. http://hdl.handle.net/10261/172054 |
Aparece en las colecciones: | (Geo3Bcn) SeisDARE |
Ficheros en este ítem:
Fichero | Descripción | Tamaño | Formato | |
---|---|---|---|---|
Descripcion_ficheros_ESCI-N.xlsx | List of the files included in this dataset | 9,54 kB | Microsoft Excel XML | Visualizar/Abrir |
Readme_ESCI-N.txt | Dataset general information | 2,51 kB | Text | Visualizar/Abrir |
Index card_ESCI-N.pdf | Index card summarizing the main characteristics of the dataset | 2,22 MB | Adobe PDF | Visualizar/Abrir |
ESCI-ZonesGeol.pdf | Map with location of the ESCI Valencia Trough, ESCI-North and ESCI Betics profiles | 67,66 kB | Adobe PDF | Visualizar/Abrir |
ESCI-N1.zip | Raw SEGY files of the ESCI-N1 profile | 1,43 GB | SEGY | Visualizar/Abrir |
ESCI-N2.zip | Raw SEGY files of the ESCI-N2 profile | 647,44 MB | SEGY | Visualizar/Abrir |
ESCI-N3.1.zip | Raw SEGY files of the ESCI-N3.1 profile | 9,96 GB | SEGY | Visualizar/Abrir |
ESCI-N3.2.zip | Raw SEGY files of the ESCI-N3.2 profile | 6,67 GB | SEGY | Visualizar/Abrir |
ESCI-N3.3.zip | Raw SEGY files of the ESCI-N3.3 profile | 9,54 GB | SEGY | Visualizar/Abrir |
ESCI-N4.zip | Raw SEGY files of the ESCI-N4 profile | 9,63 GB | SEGY | Visualizar/Abrir |
CORE Recommender
Page view(s)
512
checked on 18-abr-2024
Download(s)
367
checked on 18-abr-2024
Google ScholarTM
Check
Altmetric
Altmetric
Este item está licenciado bajo una Licencia Creative Commons