Database of multiparametric geophysical data from the TOMO-DEC experiment on Deception Island, Antarctica
Identificadores
URI: http://hdl.handle.net/10481/66391Metadatos
Mostrar el registro completo del ítemAutor
Ibáñez Godoy, Jesús Miguel; Díaz Moreno, Alejandro; Prudencio Soñora, Janire; Zandomeneghi, Daria; Wilcock, William; Barclay, Andrew; Almendros González, Francisco Javier; Benítez Ortúzar, María Del Carmen; García Yeguas, María Araceli; Alguacil De La Blanca, Ángel GerardoEditorial
Springer Nature
Materia
Geophysics Seismology Volcanology
Fecha
2017-09-12Referencia bibliográfica
Ibáñez, J., Díaz-Moreno, A., Prudencio, J. et al. Database of multi-parametric geophysical data from the TOMO-DEC experiment on Deception Island, Antarctica. Sci Data 4, 170128 (2017). [https://doi.org/10.1038/sdata.2017.128]
Patrocinador
MINECO/FEDER TEC2015-68752-R; KNOWAVES; Spanish Education and Research Ministry REN 2001-3833 CGL2005-05789-C02-02/ANT POL2006-08663 CGL2008-01660; National Science Foundation (NSF) ANT-0230094 NSF-1521855; European project MED-SUV - European Union's Seventh Framework Program 308665; European project EPOS; European Union (EU) 676564Resumen
Deception Island volcano (Antarctica) is one of the most closely monitored and studied volcanoes on the region. In January 2005, a multi-parametric international experiment was conducted that encompassed both Deception Island and its surrounding waters. We performed this experiment from aboard the Spanish oceanographic vessel 'Hesperides', and from five land-based locations on Deception Island (the Spanish scientific Antarctic base 'Gabriel de Castilla' and four temporary camps). This experiment allowed us to record active seismic signals using a large network of seismic stations that were deployed both on land and on the seafloor. In addition, other geophysical data were acquired, including bathymetric high precision multi-beam data, and gravimetric and magnetic profiles. To date, the seismic and bathymetric data have been analysed but the magnetic and gravimetric data have not. We provide P-wave arrival-time picks and seismic tomography results in velocity and attenuation. In this manuscript, we describe the main characteristics of the experiment, the instruments, the data, and the repositories from which data and information can be obtained.