Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/10110
DC Field | Value | Language |
---|---|---|
dc.contributor.authorall | Boncio, P.; Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.authorall | Pizzi, A.; Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.authorall | Brozzetti, F.; Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.authorall | Pomposo, G.; Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.authorall | Lavecchia, G.; Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.authorall | Di Naccio, D.; Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.authorall | Ferrarini, F.; Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.date.accessioned | 2015-08-06T12:01:19Z | en |
dc.date.available | 2015-08-06T12:01:19Z | en |
dc.date.issued | 2010-03-27 | en |
dc.identifier.uri | http://hdl.handle.net/2122/10110 | en |
dc.description.abstract | We provide field data of coseismic ground deformation related to the 6 April Mw 6.3 L’Aquila normal faulting earthquake. Three narrow fracture zones were mapped: Paganica‐Colle Enzano (P‐E), Mt. Castellano‐Mt. Stabiata (C‐S) and San Gregorio (SG). These zones define 13 km of surface ruptures that strike at 130–140°. We mapped four main types of ground deformation (free faces on bedrock fault scarps, faulting along synthetic splays and fissures with or without slip) that are probably due to the near‐surface lithology of the fault walls and the amount of slip that approached the surface coseismically. The P‐E and C‐S zones are characterized by downthrow to the SW (up to 10 cm) and opening (up to 12 cm), while the SG zone is characterized only by opening. Afterslip throw rates of 0.5–0.6 mm/day were measured along the Paganica fault, where paleoseismic evidence reveals recurring paleo‐earthquakes and post‐24.8 kyr slip‐rate ≥ 0.24 mm/yr. | en |
dc.language.iso | English | en |
dc.publisher.name | American Geophysical Union | en |
dc.relation.ispartof | Geophysical Research Letters | en |
dc.relation.ispartofseries | /37 (2010) | en |
dc.subject | 6 April 2009 L’Aquila earthquake | en |
dc.subject | Coseismic ground deformation | en |
dc.title | Coseismic ground deformation of the 6 April 2009 L’Aquila earthquake (central Italy, Mw6.3) | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.type.QualityControl | Peer-reviewed | en |
dc.description.pagenumber | L06308 | en |
dc.subject.INGV | 04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution | en |
dc.identifier.doi | 10.1029/2010GL042807 | en |
dc.description.obiettivoSpecifico | 2T. Tettonica attiva | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | restricted | en |
dc.relation.issn | 0094-8276 | en |
dc.relation.eissn | 1944-8007 | en |
dc.contributor.author | Boncio, P. | en |
dc.contributor.author | Pizzi, A. | en |
dc.contributor.author | Brozzetti, F. | en |
dc.contributor.author | Pomposo, G. | en |
dc.contributor.author | Lavecchia, G. | en |
dc.contributor.author | Di Naccio, D. | en |
dc.contributor.author | Ferrarini, F. | en |
dc.contributor.department | Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.department | Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.department | Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.department | Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.department | Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.department | Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | en |
dc.contributor.department | Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | 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 | Dipartimento DiSPUTer, Università di Chieti-Pescara, Italy | - |
crisitem.author.dept | DIGAT | - |
crisitem.author.dept | Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | - |
crisitem.author.dept | Università degli studi di Chieti "G. d'Annunzio" | - |
crisitem.author.dept | Geodynamics and Seismogenesis Laboratory, Dipartimento di Scienze della Terra, Università “G. d'Annunzio” | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia | - |
crisitem.author.dept | Dipartimento di Scienze della Terra, “G. d’Annunzio”Università | - |
crisitem.author.orcid | 0000-0002-5196-4956 | - |
crisitem.author.orcid | 0000-0002-0344-1173 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 04. Solid Earth | - |
Appears in Collections: | Article published / in press |
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Boncio et al_2010.pdf | main article | 809.39 kB | Adobe PDF |
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