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Thermo-Hydro-Mechanical Model and Caprock Deformation Explain the Onset of an On-going Seismo-volcanic Unrest

dc.contributor.authorAkande, Waheed Gbenga
dc.contributor.authorGan, Quan
dc.contributor.authorCornwell, Dave
dc.contributor.authorde Siena, Luca
dc.contributor.institutionUniversity of Aberdeen.Geosciencesen
dc.contributor.institutionUniversity of Aberdeen.Geology and Geophysicsen
dc.contributor.institutionUniversity of Aberdeen.Centre for Energy Transitionen
dc.date.accessioned2021-03-24T19:45:01Z
dc.date.available2021-03-24T19:45:01Z
dc.date.issued2021-03
dc.descriptionAcknowledgments The authors are grateful to the Editor, Prof. Ben‐Zion Yehuda, and the reviewers: Prof. Micol Todesco and an anonymous reviewer, whose comments and recommendations have significantly improved the quality of this work. The authors acknowledge the financial support of the Petroleum Technology Development Fund (PTDF) Nigeria for this research. The comparison of our models with monitoring data was made possible by the outstanding efforts of the staff at the INGV‐Osservatorio Vesuviano, who provide weekly information about geophysical parameters at the Campanian volcanoes (http://www.ov.ingv.it/ov/en/bollettini/272-campi-flegrei-bollettini-settimanali.html). The authors are particularly grateful to them for providing the accurate magnitude and hypocentral parameters used to create the earthquake magnitude–depth plot in this study. The authors also extend our appreciation to Prof. Derek Elsworth for his generous support in the FLAC3D software license usage.en
dc.description.statusPeer revieweden
dc.format.extent26
dc.format.extent6706618
dc.identifier188325764
dc.identifier71bcfddb-3c4e-4792-a4ba-83c26c673462
dc.identifier85103919285
dc.identifier000638091600065
dc.identifier.citationAkande, W G, Gan, Q, Cornwell, D & de Siena, L 2021, 'Thermo-Hydro-Mechanical Model and Caprock Deformation Explain the Onset of an On-going Seismo-volcanic Unrest', Journal of Geophysical Research: Solid Earth, vol. 126, no. 3, e2020JB020449. https://doi.org/10.1029/2020JB020449en
dc.identifier.doi10.1029/2020JB020449
dc.identifier.iss3en
dc.identifier.issn2169-9356
dc.identifier.otherORCID: 0000-0001-5201-8817
dc.identifier.otherORCID: 0000-0002-9843-7811
dc.identifier.otherORCID: 0000-0002-2660-027X
dc.identifier.otherORCID: /0000-0002-9843-7811/work/91891522
dc.identifier.urihttps://hdl.handle.net/2164/16117
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=85103919285&partnerID=8YFLogxKen
dc.identifier.vol126en
dc.language.isoeng
dc.relation.ispartofJournal of Geophysical Research: Solid Earthen
dc.subjectCampi Flegrei calderaen
dc.subjectcaprock deformationen
dc.subjectinduced seismicityen
dc.subjectthermo‐hydro‐mechanical modelingen
dc.subjectvolcano seismicityen
dc.subjectthermo-hydro-mechanical modelingen
dc.subjectG Geography (General)en
dc.subjectGeochemistry and Petrologyen
dc.subjectGeophysicsen
dc.subjectEarth and Planetary Sciences (miscellaneous)en
dc.subjectSpace and Planetary Scienceen
dc.subjectSupplementary Dataen
dc.subject.lccG1en
dc.titleThermo-Hydro-Mechanical Model and Caprock Deformation Explain the Onset of an On-going Seismo-volcanic Unresten
dc.typeJournal articleen

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