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A generalized theory for full microtremor horizontal-to-vertical [H/V(z, f)] spectral ratio interpretation in offshore and onshore environments

dc.creatorLontsi A.M.
dc.creatorGarcía-Jerez A.
dc.creatorMolina-Villegas J.C.
dc.creatorSánchez-Sesma F.J.
dc.creatorMolkenthin C.
dc.creatorOhrnberger M.
dc.creatorKrüger F.
dc.creatorWang R.
dc.creatorFäh D.
dc.date2019
dc.date.accessioned2020-04-29T14:53:55Z
dc.date.available2020-04-29T14:53:55Z
dc.identifier.issn0956540X
dc.identifier.urihttp://hdl.handle.net/11407/5760
dc.descriptionAdvances in the field of seismic interferometry have provided a basic theoretical interpretation to the full spectrum of the microtremor horizontal-to-vertical spectral ratio [H/V(f)]. The interpretation has been applied to ambient seismic noise data recorded both at the surface and at depth. The new algorithm, based on the diffuse wavefield assumption, has been used in inversion schemes to estimate seismic wave velocity profiles that are useful input information for engineering and exploration seismology both for earthquake hazard estimation and to characterize surficial sediments. However, until now, the developed algorithms are only suitable for on land environments with no offshore consideration. Here, the microtremor H/V(z, f) modelling is extended for applications to marine sedimentary environments for a 1-D layered medium. The layer propagator matrix formulation is used for the computation of the required Green's functions. Therefore, in the presence of a water layer on top, the propagator matrix for the uppermost layer is defined to account for the properties of the water column. As an application example we analyse eight simple canonical layered earth models. Frequencies ranging from 0.2 to 50 Hz are considered as they cover a broad wavelength interval and aid in practice to investigate subsurface structures in the depth range from a few meters to a few hundreds of meters. Results show a marginal variation of 8 per cent at most for the fundamental frequency when a water layer is present. The water layer leads to variations in H/V peak amplitude of up to 50 per cent atop the solid layers. © The Author(s) 2019.
dc.language.isoeng
dc.publisherOxford University Press
dc.relation.isversionofhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85075640474&doi=10.1093%2fgji%2fggz223&partnerID=40&md5=7ce964f4b24f726f5caec87cc0583a7a
dc.sourceGeophysical Journal International
dc.subjectEarthquake hazards
dc.subjectNumerical modelling
dc.subjectSeismic interferometry
dc.subjectSite effects
dc.subjectTheoretical seismology
dc.subjectWave propagation
dc.subjectComputation theory
dc.subjectHazards
dc.subjectInterferometry
dc.subjectMarine applications
dc.subjectMatrix algebra
dc.subjectNumerical models
dc.subjectOffshore oil well production
dc.subjectSurficial sediments
dc.subjectWave propagation
dc.subjectEarthquake hazard
dc.subjectExploration seismology
dc.subjectFundamental frequencies
dc.subjectHorizontal-to-vertical spectral ratios
dc.subjectSedimentary environment
dc.subjectSeismic interferometries
dc.subjectSite effects
dc.subjectTheoretical seismologies
dc.subjectEarthquakes
dc.subjectalgorithm
dc.subjectGreen function
dc.subjectmarine environment
dc.subjectmicrotremor
dc.subjectnumerical model
dc.subjectoffshore structure
dc.subjectradar interferometry
dc.subjectseismic hazard
dc.subjectsite effect
dc.subjectsurficial sediment
dc.subjecttheoretical study
dc.subjectwave propagation
dc.titleA generalized theory for full microtremor horizontal-to-vertical [H/V(z, f)] spectral ratio interpretation in offshore and onshore environments
dc.typeArticleeng
dc.rights.accessrightsinfo:eu-repo/semantics/restrictedAccess
dc.publisher.programIngeniería Civil
dc.identifier.doi10.1093/gji/ggz223
dc.relation.citationvolume218
dc.relation.citationissue2
dc.relation.citationstartpage1276
dc.relation.citationendpage1297
dc.publisher.facultyFacultad de Ingenierías
dc.affiliationLontsi, A.M., Swiss Seismological Service, ETH Zürich, Zurich, 8092, Switzerland; García-Jerez, A., Departamento de Química y Física, Universidad de Almeria, Almeria, 04120, Spain, Instituto Andaluz de Geofísica, Universidad de Granada, Granada, 18071, Spain; Molina-Villegas, J.C., Facultad de Ingenierías, Universidad de Medellín, Carrera 87 No 30-65, Medellín, Colombia, Departamento de Ingeniería Civil, Facultad de Minas, Universidad Nacional de Colombia - Sede Medellín, Carrera 80 No 65-223, Medellín, Colombia; Sánchez-Sesma, F.J., Instituto de Ingeniería, Universidad Nacional Autónoma de México, Circuito Escolar s/n, Cd Universitaria, Coyoacán, Cdmx, 04510, Mexico; Molkenthin, C., Institute of Mathematics, University of Potsdam, Potsdam, 14476, Germany; Ohrnberger, M., Institute of Earth and Environmental Science, University of Potsdam, Potsdam, 14476, Germany; Krüger, F., Institute of Earth and Environmental Science, University of Potsdam, Potsdam, 14476, Germany; Wang, R., GFZ German Research Centre for Geosciences, Potsdam, 14473, Germany; Fäh, D., Swiss Seismological Service, ETH Zürich, Zurich, 8092, Switzerland
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