Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/14280
DC Field | Value | Language |
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dc.date.accessioned | 2021-01-19T14:10:27Z | - |
dc.date.available | 2021-01-19T14:10:27Z | - |
dc.date.issued | 2021 | - |
dc.identifier.uri | http://hdl.handle.net/2122/14280 | - |
dc.description.abstract | We have reinterpreted the causative fault parameters of the 2005 Zarand earthquake in the light of a new imagery study using Interferometric Synthetic Aperture Radar (InSAR). By conducting a joint inversion of two InSAR datasets, we can characterize the rupture as it relates to complex local structures. At first, the mainshock ruptured a nearly pure reverse fault, dipping ~65° NNW in the basement below the southeastern area of Zarand. Two more fault segments were subsequently activated: an oblique‐normal fault segment parallel to the first segment, dipping 61° to the south, and a normal‐oblique fault segment at the eastern termination of the rupture zone. The first fault segment ruptured the surface, while slip along the other two segments was confined to the lower sedimentary strata. | en_US |
dc.language.iso | English | en_US |
dc.publisher.name | Wiley | en_US |
dc.relation.ispartof | Terra Nova | en |
dc.relation.ispartofseries | 3/33 (2021) | en_US |
dc.title | Multiple source analysis from InSAR data and new insights into fault activation: The 2005 Zarand, Iran, earthquake | en_US |
dc.type | article | en |
dc.description.status | Published | en_US |
dc.type.QualityControl | Peer-reviewed | en_US |
dc.description.pagenumber | 274-283 | en_US |
dc.identifier.doi | 10.1111/ter.12513 | en_US |
dc.description.obiettivoSpecifico | 2T. Deformazione crostale attiva | en_US |
dc.description.journalType | JCR Journal | en_US |
dc.contributor.author | Golshadi, Zeinab | - |
dc.contributor.author | Rezapour, Mehdi | - |
dc.contributor.author | Atzori, Simone | - |
dc.contributor.author | Salvi, Stefano | - |
dc.contributor.department | Institute of Geophysics, University of Tehran, Tehran, Iran | en_US |
dc.contributor.department | Institute of Geophysics, University of Tehran, Tehran, Iran | en_US |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | en_US |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | en_US |
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 | Institute of Geophysics, University of Tehran, Tehran, Iran | - |
crisitem.author.dept | Institute of Geophysics, University of Tehran, Tehran, Iran | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | - |
crisitem.author.orcid | 0000-0002-8112-7083 | - |
crisitem.author.orcid | 0000-0002-5031-9904 | - |
crisitem.author.orcid | 0000-0002-7776-6544 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.author.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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Golshadi et al 2020 (Zarand, Iran) - Terra Nova.pdf | 1.23 MB | Adobe PDF |
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