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Database of multiparametric geophysical data from the TOMO-DEC experiment on Deception Island, Antarctica
Database of multiparametric geophysical data from the TOMO-DEC experiment on Deception Island, Antarctica
We are grateful to the officers and crew of the Spanish vessels 'R/V Hesperides' and 'R/V Las Palmas', the personnel of the Marine Technology Unit (UTM), the military personnel of the 'Gabriel de Castilla' Spanish base, and the members of the TOMODEC Working Group. This manuscript has been partially funded by the following research projects: the Spanish project TEC2015-68752-R (MINECO/FEDER); KNOWAVES; the Spanish Education and Research Ministry grants REN 2001-3833, CGL2005-05789-C02-02/ANT, POL2006-08663, and CGL2008-01660; the U.S. National Science Foundation grant ANT-0230094; the European project MED-SUV funded by the European Union's Seventh Framework Program for research, technological development and demonstration under grant agreement No 308665; the European project EPOS; the European Union's Horizon 2020 research and innovation programme under grant agreement No 676564; and the U.S. National Science Foundation grant NSF-1521855 Hazard SEES project. Ocean bottom seismometers were provided by the U.S National Oceanographic Instrument Pool. This publication reflects only the authors' views. The European Commission is not responsible for any use that may be made of the information it contains.
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.
Spanish Education and Research Ministry REN 2001-3833 CGL2005-05789-C02-02/ANT POL2006-08663 CGL2008-01660
European project MED-SUV - European Union's Seventh Framework Program 308665
National Science Foundation (NSF) ANT-0230094 NSF-1521855
MINECO/FEDER TEC2015-68752-R
European Union (EU) 676564
European project EPOS
KNOWAVES
- State University of New York at Potsdam United States
- University of Granada Spain
- Washington State University United States
Geophysics, Volcanology, Seismology
Geophysics, Volcanology, Seismology
4815
1. Ibáñez, J. M., Díaz-Moreno, A., Prudencio, J. & Abramenkov, S. TOMO-ETNA experiment at Etna volcano: activities on land. Annals of Geophysics 59, 1-21 (2016).
2. Zollo, A. et al. 2D seismic tomography of Somma-Vesuvius. Description of the experiment and preliminary results. Annals of Geophysics 39 (1996).
3. Zollo, A. et al. Evidence for the buried rim of Campi Flegrei caldera from 3-d active seismic imaging. Geophysical Research Letters 30 (2003).
4. Martí, J., Geyer, A. & Aguirre-Diaz, G. Origin and evolution of the Deception island caldera (South Shetland Islands, Antarctica). Bulletin of Volcanology 75, 1-18 (2013).
5. Torrecillas, C., Berrocoso, M., Felpeto, A., Torrecillas, M. D. & Garcia, A. Reconstructing palaeo-volcanic geometries using a Geodynamic Regression Model (GRM): Application to Deception Island volcano (South Shetland Islands, Antarctica). Geomorphology 182, 79-88 (2013).
6. Ibáñez, J. M. et al. Seismo volcanic signals at Deception Island volcano (Antarctica): wavefield analysis and source modeling. Journ. Geophy. Res. 105, n° 6 13905-13931 (2000).
7. Ibáñez, J. M., Almendros, J., Carmona, E., Martínez-Arévalo, C. & Abril, M. The recent seismo-volcanic activity at Deception Island volcano. Deep-Sea Research, Part II. In a special vol. ERUPT: Ecosystem studies of an enclosed bay within Deception Island, Antarctica, ed. K. Smith. 50, 1611-1629 (2003).
8. Ibáñez, J. M. et al. The 1998-1999 seismic series at Deception Island volcano, Antarctica. Journ. Vol. Geo. Res. 128, 65-88 (2003).
9. Carmona, E., Almendros, J., Peña, J. A. & Ibáñez, J. M. Characterization of fracture systems using precise array locations of earthquake multiplets: An example at Deception Island volcano. Antarctica. Journ. Geophys. Res 115, 1-20 (2010).
10. Carmona, E., Almendros, J., Serrano, I., Stich, D. & Ibáñez, J. M. Results from seismic monitoring surveys at Deception Island Volcano (Antarctica) from 1999 to 2011. Antarctic Science. 24, 485-499 (2012).
citations This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).0 popularity This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.Average influence This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).Average impulse This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.Average citations This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).0 popularity This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.Average influence This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).Average impulse This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.Average
Citations provided by BIP!Popularity provided by BIP!- National Science Foundation (NSF)
- 0230094
- Directorate for Geosciences | Division of Polar Programs
- National Science Foundation (NSF)
- 1521855
- State University of New York at Potsdam United States
- University of Granada Spain
- Washington State University United States
We are grateful to the officers and crew of the Spanish vessels 'R/V Hesperides' and 'R/V Las Palmas', the personnel of the Marine Technology Unit (UTM), the military personnel of the 'Gabriel de Castilla' Spanish base, and the members of the TOMODEC Working Group. This manuscript has been partially funded by the following research projects: the Spanish project TEC2015-68752-R (MINECO/FEDER); KNOWAVES; the Spanish Education and Research Ministry grants REN 2001-3833, CGL2005-05789-C02-02/ANT, POL2006-08663, and CGL2008-01660; the U.S. National Science Foundation grant ANT-0230094; the European project MED-SUV funded by the European Union's Seventh Framework Program for research, technological development and demonstration under grant agreement No 308665; the European project EPOS; the European Union's Horizon 2020 research and innovation programme under grant agreement No 676564; and the U.S. National Science Foundation grant NSF-1521855 Hazard SEES project. Ocean bottom seismometers were provided by the U.S National Oceanographic Instrument Pool. This publication reflects only the authors' views. The European Commission is not responsible for any use that may be made of the information it contains.
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.
Spanish Education and Research Ministry REN 2001-3833 CGL2005-05789-C02-02/ANT POL2006-08663 CGL2008-01660
European project MED-SUV - European Union's Seventh Framework Program 308665
National Science Foundation (NSF) ANT-0230094 NSF-1521855
MINECO/FEDER TEC2015-68752-R
European Union (EU) 676564
European project EPOS
KNOWAVES