Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/8614
DC Field | Value | Language |
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dc.contributor.authorall | Cianchini, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.authorall | De Santis, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.authorall | Barraclough, D. R.; British Geological Survey, Edinburgh, UK | en |
dc.contributor.authorall | Wu, L. X.; Academy of Disaster Reduction and Emergency Management, Beijing Normal University, China | en |
dc.contributor.authorall | Qin, K.; China University of Mining and Technology, Beijing, China | en |
dc.date.accessioned | 2013-04-12T09:58:16Z | en |
dc.date.available | 2013-04-12T09:58:16Z | en |
dc.date.issued | 2012-07-23 | en |
dc.identifier.uri | http://hdl.handle.net/2122/8614 | en |
dc.description.abstract | With the aim of obtaining a deeper knowledge of the physical phenomena associated with the 2009 L’Aquila (Central Italy) seismic sequence, culminating with a Mw = 6.3 earthquake on 6 April 2009, and possibly of identifying some kind of earthquake-related magnetic or geoelectric anomaly, we analyse the geomagnetic field components measured at the magnetic observatory of L’Aquila and their variations in time. In particular, trends of magnetic transfer functions in the years 2006–2010 are inspected. They are calculated from the horizontal to vertical magnetic component ratio in the frequency domain, and are very sensitive to deep and lateral geoelectric characteristics of the measurement site. Entropy analysis, carried out from the transfer functions with the so called transfer function entropy, points out clear temporal burst regimes of a few distinct harmonics preceding the main shock of the seismic sequence. A possible explanation is that they could be related to deep fluid migrations and/or to variations in the micro-/meso-fracturing that affected significantly the conductivity (ordered/disordered) distribution in a large lithospheric volume under the seismogenic layer below L’Aquila area. This interpretation is also supported by the analysis of hypocentres depths before the main shock occurrence. | en |
dc.language.iso | English | en |
dc.publisher.name | Copernicus Publications | en |
dc.relation.ispartof | Nonlinear Processes in Geophysics | en |
dc.relation.ispartofseries | / 19 (2012) | en |
dc.subject | earthquake event | en |
dc.subject | earthquake hypocenter | en |
dc.subject | earthquake magnitude | en |
dc.subject | entropy | en |
dc.subject | fluid mechanics | en |
dc.subject | geomagnetic field | en |
dc.subject | seismicity | en |
dc.subject | Abruzzi | en |
dc.subject | Italy | en |
dc.subject | L'Aquila | en |
dc.subject | Aquila | en |
dc.title | Magnetic transfer function entropy and the 2009 Mw = 6.3 L’Aquila earthquake (Central Italy) | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | 401-409 | en |
dc.subject.INGV | 04. Solid Earth::04.02. Exploration geophysics::04.02.04. Magnetic and electrical methods | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics | en |
dc.identifier.doi | 10.5194/npg-19-401-2012 | en |
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dc.description.obiettivoSpecifico | 1.6. Osservazioni di geomagnetismo | en |
dc.description.obiettivoSpecifico | 3.1. Fisica dei terremoti | en |
dc.description.obiettivoSpecifico | 3.4. Geomagnetismo | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | open | en |
dc.relation.issn | 1023-5809 | en |
dc.relation.eissn | 1607-7946 | en |
dc.contributor.author | Cianchini, G. | en |
dc.contributor.author | De Santis, A. | en |
dc.contributor.author | Barraclough, D. R. | en |
dc.contributor.author | Wu, L. X. | en |
dc.contributor.author | Qin, K. | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia | en |
dc.contributor.department | British Geological Survey, Edinburgh, UK | en |
dc.contributor.department | Academy of Disaster Reduction and Emergency Management, Beijing Normal University, China | en |
dc.contributor.department | China University of Mining and Technology, Beijing, China | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
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 Roma2, Roma, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia | - |
crisitem.author.dept | British Geological Survey, Edinburgh, U. K. | - |
crisitem.author.dept | China University of Mining and Technology, School of Environment Science and Spatial Informatics, Xuzhou, China | - |
crisitem.author.dept | China University of Mining & Technology (Beijing) | - |
crisitem.author.orcid | 0000-0003-2832-0068 | - |
crisitem.author.orcid | 0000-0002-3941-656X | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.classification.parent | 04. Solid Earth | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
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Cianchini-G._Magnetic-transfer-function-entropy.NPG.2012.pdf | 2.48 MB | Adobe PDF | View/Open |
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