Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/1184
DC Field | Value | Language |
---|---|---|
dc.contributor.authorall | Marzocchi, W.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia | en |
dc.contributor.authorall | Zaccarelli, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.authorall | Boschi, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italia | en |
dc.date.accessioned | 2006-06-28T14:12:45Z | en |
dc.date.available | 2006-06-28T14:12:45Z | en |
dc.date.issued | 2004-02-17 | en |
dc.identifier.uri | http://hdl.handle.net/2122/1184 | en |
dc.description.abstract | A correlation has been recently found between large earthquakes and the succeeding largest 9 explosive eruptions of the last century, which has been interpreted as a product of co- and post-seismic stress diffusion. Here, we check the statistical significance of the proposed coupling by using a larger dataset, and investigate the reliability of the causality hypothesis. We find that the volcanoes with VEI ≥ 4 eruptions underwent, in the few decades before the volcanic event, higher seismic stress perturbations due to large earthquakes compared to other volcanic areas. The correlation is statistically significant and it is not explained by a spatio-temporal clustering of eruptions and earthquakes due to tectonic pulses. This implies that the large earthquakes indeed triggered the eruptions. | en |
dc.description.sponsorship | Gruppo Nazionale di Vulcanologia and e-Ruption projects | en |
dc.format.extent | 1019925 bytes | en |
dc.format.mimetype | application/pdf | en |
dc.language.iso | English | en |
dc.publisher.name | AGU | en |
dc.relation.ispartof | Geophysical Research Letters | en |
dc.relation.ispartofseries | 31/4(2004) | en |
dc.subject | Volcanology | en |
dc.subject | Eruption mechanisms | en |
dc.subject | Seismology | en |
dc.subject | Volcano seismology | en |
dc.subject | Tectonophysics | en |
dc.subject | Stresses - general | en |
dc.title | Phenomenological evidence in favor of a remote seismic coupling for large volcanic eruptions | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.identifier.URL | http://www.agu.org/pubs/crossref/2004.../2003GL018709.shtml | en |
dc.subject.INGV | 05. General::05.01. Computational geophysics::05.01.04. Statistical analysis | en |
dc.identifier.doi | 10.1029/2003GL018709 | en |
dc.description.fulltext | reserved | en |
dc.contributor.author | Marzocchi, W. | en |
dc.contributor.author | Zaccarelli, L. | en |
dc.contributor.author | Boschi, E. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Bologna, Bologna, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italia | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Bologna, Bologna, Italia | - |
crisitem.author.orcid | 0000-0002-9114-1516 | - |
crisitem.author.orcid | 0000-0002-4053-7625 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 05. General | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
Files in This Item:
File | Description | Size | Format | Existing users please Login |
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marzocchi-et-al_grl-2004.pdf | 421.68 kB | Adobe PDF |
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