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http://hdl.handle.net/10261/266338
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dc.contributor.author | Handoyo, Handoyo | es_ES |
dc.contributor.author | Alcalde, Juan | es_ES |
dc.contributor.author | DeFelipe, Irene | es_ES |
dc.contributor.author | Palomeras, Imma | es_ES |
dc.contributor.author | Martín-Banda, R. | es_ES |
dc.contributor.author | García Mayordomo, Julián | es_ES |
dc.contributor.author | Martí, David | es_ES |
dc.contributor.author | Martínez-Díaz, J. J. | es_ES |
dc.contributor.author | Insúa Arévalo, Juan Miguel | es_ES |
dc.contributor.author | Teixidó, T. | es_ES |
dc.contributor.author | Marzán, Ignacio | es_ES |
dc.contributor.author | Carbonell, Ramón | es_ES |
dc.date.accessioned | 2022-04-05T12:01:17Z | - |
dc.date.available | 2022-04-05T12:01:17Z | - |
dc.date.issued | 2022-04 | - |
dc.identifier.citation | Applied Sciences, 12(7): 3398 (2022) | es_ES |
dc.identifier.uri | http://hdl.handle.net/10261/266338 | - |
dc.description.abstract | The critical zone (CZ) represents the most-shallow subsurface, where the bio-, hydro-, and geospheres interact with anthropogenic activity. To characterize the thickness and lateral variations of the CZ, here we focus on the Eastern Betic Shear Zone (EBSZ), one of the most tectonically active regions in the Iberian Peninsula. Within the EBSZ, the Guadalentín Depression is a highly populated area with intensive agricultural activity, where the characterization of the CZ would provide valuable assets for land use management and seismic hazard assessments. To achieve this, we have conducted an interdisciplinary geophysical study along the eastern border of the Guadalentín Depression to characterize the CZ and the architecture of the shallow subsurface. The datasets used include Electrical Resistivity Tomography (ERT), first-arrival travel time seismic tomography, and multichannel analysis of surface waves (MASW). The geophysical datasets combined help to constrain the high-resolution structure of the subsurface and image active fault systems along four transects. The resulting geophysical models have allowed us to interpret the first ~150 m of the subsurface and has revealed: (i) the variable thickness of the CZ; (ii) the CZ relationship between the fault zone and topographic slope; and (iii) the differences in CZ thickness associated with the geological units. Our results provide a method for studying the shallow subsurface of active faults, complementing previous geological models based on paleo-seismological trenches, and can be used to improve the CZ assessment of tectonically active regions. | es_ES |
dc.description.sponsorship | The authors would like to thank the following: The project INTERGEO (CGL2013-47412-C2-1-P) GEO3BCN-CSIC for providing access to the data. SeisDARE provides public access to the seismic data [86]. The KEMDIKBUDRISTEK of the Republic of Indonesia for providing a Ph.D. scholarship to the first author. The GIPP-GFZ (Germany) and Lisbon University (Portugal) provided the instrumentation. Additionally, we sincerely thank Seismic Unix CWP (Center for Wave Phenomena, Colorado School of Mines) for allowing us to use the free academic license software, and we also thank everyone who was directly or indirectly involved in this work. J.A. is funded by grant IJC2018-036074-I and by MCIN/AEI /10.13039/501100011033. I.P. is funded by the Spanish Government and the Universidad de Salamanca (Beatriz Galindo grant BEGAL 18/00090). This project was funded by Grant 2017SGR1022 (GREG) from the Generalitat de Catalunya (AGAUR); EU (H2020) 871121 (EPOS-SP); and EIT-RawMaterias 17024 from the European Institute of Technology (EIT) (SIT4ME). | es_ES |
dc.language.iso | eng | es_ES |
dc.publisher | Multidisciplinary Digital Publishing Institute | es_ES |
dc.relation | info:eu-repo/grantAgreement/MINECO//CGL2013-47412-C2-1-P/ES/ANALISIS DEL POTENCIAL SISMICO DE LAS ZONAS INTERSEGMENTO DE FALLAS DE DESGARRE MEDIANTE ANALISIS Y MONITOREO GEOLOGICO, GEODESICO Y GEOFISICO/ | es_ES |
dc.relation | Plan Estatal de investigación Científica y Técnica y de Innovación 2021-2023MCIN/AEI /10.13039/501100011033 | es_ES |
dc.relation.isversionof | Publisher's version | es_ES |
dc.rights | openAccess | es_ES |
dc.subject | MASW | es_ES |
dc.subject | Tomography | es_ES |
dc.subject | ERT | es_ES |
dc.subject | Fault | es_ES |
dc.subject | Critical zone (CZ) | es_ES |
dc.title | Geophysical Imaging of the Critical Zone along the Eastern Betic Shear Zone (EBSZ), SE Iberian Peninsula | es_ES |
dc.type | artículo | es_ES |
dc.identifier.doi | 10.3390/app12073398 | - |
dc.description.peerreviewed | Peer reviewed | es_ES |
dc.relation.publisherversion | https://doi.org/10.3390/app12073398 | es_ES |
dc.identifier.e-issn | 2076-3417 | - |
dc.rights.license | https://creativecommons.org/licenses/by/4.0/ | es_ES |
dc.contributor.funder | Ministerio de Economía y Competitividad (España) | es_ES |
dc.contributor.funder | Generalitat de Catalunya | es_ES |
dc.contributor.funder | EIT RawMaterials | es_ES |
dc.contributor.funder | Ministerio de Ciencia, Innovación y Universidades (España) | es_ES |
dc.relation.csic | Sí | es_ES |
oprm.item.hasRevision | no ko 0 false | * |
dc.identifier.funder | http://dx.doi.org/10.13039/501100002809 | es_ES |
dc.identifier.funder | http://dx.doi.org/10.13039/501100003329 | es_ES |
dc.contributor.orcid | Martí, David [0000-0002-5502-921X] | es_ES |
dc.contributor.orcid | Carbonell, Ramón [0000-0003-2019-1214] | es_ES |
dc.contributor.orcid | Alcalde, Juan [0000-0001-9806-5600] | es_ES |
dc.contributor.orcid | DeFelipe, Irene [0000-0003-0367-234X] | es_ES |
dc.type.coar | http://purl.org/coar/resource_type/c_6501 | es_ES |
item.openairetype | artículo | - |
item.languageiso639-1 | en | - |
item.grantfulltext | open | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
item.cerifentitytype | Publications | - |
Aparece en las colecciones: | (Geo3Bcn) Artículos (IGME) Artículos |
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Alcalde_applsci-12-03398-v2.pdf | 9,13 MB | Adobe PDF | Visualizar/Abrir |
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