3D shear-wave velocity structure for Oran city, northwestern Algeria, from inversion of ambient vibration single-station and array measurements
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Campo DC | Valor | Idioma |
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dc.contributor | Grupo de Ingeniería y Riesgo Sísmico (GIRS) | es_ES |
dc.contributor.author | Saadi, Ahmed | - |
dc.contributor.author | Issaadi, Abdelouahab | - |
dc.contributor.author | Semmane, Fethi | - |
dc.contributor.author | Yelles-Chaouche, Abdelkrim | - |
dc.contributor.author | Galiana-Merino, Juan José | - |
dc.contributor.author | Layadi, Khalissa | - |
dc.contributor.author | Chimouni, Redouane | - |
dc.contributor.other | Universidad de Alicante. Departamento de Física, Ingeniería de Sistemas y Teoría de la Señal | es_ES |
dc.contributor.other | Universidad de Alicante. Instituto Universitario de Física Aplicada a las Ciencias y las Tecnologías | es_ES |
dc.date.accessioned | 2022-10-17T09:13:54Z | - |
dc.date.available | 2022-10-17T09:13:54Z | - |
dc.date.issued | 2022-10-10 | - |
dc.identifier.citation | Soil Dynamics and Earthquake Engineering. 2023, 164: 107570. https://doi.org/10.1016/j.soildyn.2022.107570 | es_ES |
dc.identifier.issn | 0267-7261 (Print) | - |
dc.identifier.issn | 1879-341X (Online) | - |
dc.identifier.uri | http://hdl.handle.net/10045/128504 | - |
dc.description.abstract | The city of Oran experienced several earthquakes. Therefore, the characterization of its subsurface is crucial for a better evaluation of the seismic hazard. Using ambient vibration single-station and array measurements at 193 sites, the HVSR curves showed a variation of the fundamental frequency peak between 0.3 and 7.4 Hz, growing towards the west, with maximum amplitude of ∼6. The shallow structure has been explored by means of F–K analysis. Joint inversion of the HVSR and Rayleigh wave dispersion curves showed 3 layers of soft and stiff sediments of varying thicknesses overlying the bedrock. The shear-wave velocity (Vs) of the sediments varies between 280 and 1300 m/s and that of the bedrock can reach 2500 m/s. Cross sections show a decrease in sediments thickness from east to west where bedrock outcrops. The maximum depth of bedrock is 1050 m northeast of the city. The obtained Vs models support a soil classification ranging from stiff soil to hard rock. | es_ES |
dc.language | eng | es_ES |
dc.publisher | Elsevier | es_ES |
dc.rights | © 2022 Elsevier Ltd. | es_ES |
dc.subject | Ambient vibrations | es_ES |
dc.subject | HVSR | es_ES |
dc.subject | Array technique | es_ES |
dc.subject | F–K analysis | es_ES |
dc.subject | Vs-structure | es_ES |
dc.subject | Oran city | es_ES |
dc.title | 3D shear-wave velocity structure for Oran city, northwestern Algeria, from inversion of ambient vibration single-station and array measurements | es_ES |
dc.type | info:eu-repo/semantics/article | es_ES |
dc.peerreviewed | si | es_ES |
dc.identifier.doi | 10.1016/j.soildyn.2022.107570 | - |
dc.relation.publisherversion | https://doi.org/10.1016/j.soildyn.2022.107570 | es_ES |
dc.rights.accessRights | info:eu-repo/semantics/embargoedAccess | es_ES |
dc.date.embargoEnd | info:eu-repo/date/embargoEnd/2024-10-11 | - |
Aparece en las colecciones: | INV - GIRS - Artículos de Revistas |
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Archivo | Descripción | Tamaño | Formato | |
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Saadi_etal_2022_SoilDynamEarthquakeEng_final.pdf | Versión final (acceso restringido) | 13,97 MB | Adobe PDF | Abrir Solicitar una copia |
Saadi_etal_2022_SoilDynamEarthquakeEng_revised.pdf | Embargo 24 meses (acceso abierto: 11 oct. 2024) | 2,33 MB | Adobe PDF | Abrir Solicitar una copia |
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