| A new closed analytical solution for the elastodynamic half-space Green’s function |
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| On the Utility of Horizontal-to-Vertical Spectral Ratios of Ambient Noise in Joint Inversion with Rayleigh Wave Dispersion Curves for the Large-N Maupasacq Experiment |
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| Horizontal-to-Vertical Spectral Ratio of Ambient Vibration Obtained with Hilbert–Huang Transform |
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| Campo eléctrico en un aislante calculado como un valor medio |
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| Use of peaks and troughs in the horizontal-to-vertical spectral ratio of ambient noise for Rayleigh-wave dispersion curve picking |
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| Imaging the structure of the Sun Pyramid (Teotihuacán, Mexico) from passive seismic methods |
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| Modeling the two- and three-dimensional displacement field in Lorca, Spain, subsidence and the global implications |
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| The inversion of spectral ratio H/V in a layered system using the diffuse field assumption (DFA) |
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| Surface dynamic deformation estimates from local seismicity: the Itoiz reservoir, Spain |
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| A computer code for forward calculation and inversion of the H/V spectral ratio under the diffuse field assumption |
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| Numerical simulation of multiple scattering of P and SV waves caused by near-surface parallel cracks |
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| Identification of T-Waves in the Alboran Sea |
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| Structure of Alluvial Valleys from 3-D Gravity Inversion: The Low Andarax Valley (Almeria, Spain) Test Case |
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| Current Topics on Deformation Monitoring and Modelling, Geodynamics and Natural Hazards: Introduction |
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| Source Parameters of Earthquakes Recorded Near the Itoiz Dam (Northern Spain) |
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| Using diffuse field theory to interpret the H/V spectral ratio from earthquake records in Cibeles seismic station, Mexico City |
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| Earth Models at the Low Andarax River Valley (SE Spain) by Means of Cross-Correlation of Ambient Noise |
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| Theory and simulation of time-fractional fluid diffusion in porous media |
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| Diffuse elastic wavefield within a simple crustal model. Some consequences for low and high frequencies |
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| Some properties of the Green's function of simplified elastodynamic problems |
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| Seismic Hazard and Ground Motion Characterization at the Itoiz Dam (Northern Spain) |
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| Weighted complex networks applied to seismicity: The Itoiz dam (Northern Spain) |
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| A theory for microtremor H/V spectral ratio: Application for a layered medium |
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| Shallow structure of Deception Island, Antarctica, from correlations of ambient seismic noise on a set of dense seismic arrays |
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| Diffuse seismic waves and site effects |
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| Energy partitions among elastic waves for dynamic surface loads in a semi-infinite solid |
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| A subsurface stress analysis and its possible relation with seismicity near the Itoiz Reservoir, Navarra, Northern Spain |
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| Assessing the reliability of the single circular-array method for love-wave ambient-noise surveying |
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| Numerical modelling of pore pressure variations due to time varying loads using a hybrid technique: The case of the Itoiz reservoir (Northern Spain) |
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| Interferometría radar aplicada a terremotos de magnitud moderada en las Cordilleras Béticas, SO España |
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| Analysis of complex networks associated to seismic clusters near the Itoiz reservoir dam |
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| In-plane seismic response of inhomogeneous alluvial valleys with vertical gradients of velocities and constant Poisson ratio |
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| Mie elastic scattering generated by cracks |
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| Stress relations in three recent seismic series in the Murcia region, southeastern Spain |
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| An alternative method for calculation of Rayleigh and Love wave phase velocities by using three-component records on a single circular array without a central station |
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| Boundary element simulation of scattering of elastic waves by 3-D cracks |
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| Non extensivity in meteor showers |
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| Determination of elastic properties of shallow sedimentary deposits applying a spatial autocorrelation method |
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| Diffuse fields in dynamic elasticity |
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| Retrieval of elastic green's tensor near a cylindrical inhomogeneity from vector correlations |
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| Three-dimensional indirect boundary element method for deformation and gravity changes in volcanic areas: Application to Teide volcano (Tenerife, Canary Islands) |
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| Some insights into topographic, elastic and self-gravitation interaction in modelling ground deformation and gravity changes in active volcanic areas |
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| Shallow velocity structure using joint inversion of array and h/v spectral ratio of ambient noise: The case of Mula town (SE of Spain) |
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| Scattering of elastic waves in cracked media using a finite difference method |
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| Topography and self-gravitation interaction in elastic-gravitational modeling |
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| Shear-wave velocity structure around Teide volcano: Results using microtremors with the SPAC method and implications for interpretation of geodetic results |
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| Multiple scattering of elastic waves by subsurface fractures and cavities |
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| Elastodynamic 2D Green function retrieval from cross-correlation: Canonical inclusion problem |
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| Characterization of the sedimentary cover of the Zafarraya basin, southern Spain, by means of ambient noise |
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| On the relative importance of self-gravitation and elasticity in modeling volcanic ground deformation and gravity changes |
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| Evaluation of local site effect in mula town (Murcia, Spain) applicable to seismic risk management |
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| Modelling Gravity changes and crustal deformation in active volcanic areas |
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| Simulation of an irregular free surface with a displacement finite-difference scheme |
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| Diffraction of seismic waves in an elastic, cracked halfplane using a boundary integral formulation |
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| On the correlation of seismic microtremors |
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| The use of ambient seismic noise measurements for the estimation of surface soil effects: The Motril City case (Southern Spain) |
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| Simulation of the seismic response of sedimentary basins with vertical constant-gradient velocity for incident SH waves |
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| Microtremor analyses at Teide Volcano (Canary Islands, Spains): Assessment of natural frequencies of vibration using time-dependent horizontal-to-vertical spectral ratios |
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| Three-dimesional simulation of ground motion in the Zafarraya Basin (Southern Spain) up to 1.335 Hz under incident plane waves |
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| Propagation of SH elastic waves in deep sedimentary basins with an oblique velocity gradient |
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| InSAR volcano and seismic monitoring in Spain. Results for the period 1992-2000 and possible interpretations |
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| 3D seismic response of the deep basement structure of the Granada Basin (southern Spain) |
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| Surface soil effects study using short-period microtremor observations in Almería City, Southern Spain |
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| A numerical experiment on the horizontal to vertical spectral ratio in flat sedimentary basins |
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| On the horizontal-to-vertical spectral ratio in sedimentary basins |
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| Seismic response of 3D topographical irregularities under incoming elastic waves from point sources |
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| Computing topographical 3D site effects using a fast IBEM/conjugate gradient approach |
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| Regional seismic activity around Livingston and Deception islands from 1992 to 1996: shallow and intermediate-depth earthquakes |
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| Diffraction of P, S and Rayleigh waves by three-dimensional topographies |
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| Reply to comment by J. L. Mateos, O. Novaro, T. H. Seligman and J. Flores on 'Can horizontal P waves be trapped and resonate in a shallow sedimentary basin?' |
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| Seismic source parameters for microearthquakes of the Granada basin (southern Spain) |
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| Can horizontal P waves be trapped and resonate in a shallow sedimentary basin? |
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| Seismic response of three-dimensional alluvial valleys for incident P,S, and Rayleigh waves |
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| Simulation of the seismic response of a 2D sedimentary basin: a comparison between the indirect boundary element method and a hybrid technique |
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| Spatial and temporal analysis of a seismic series using a new version of the three point method: application to the 1989 Antequera (Spain) earthquakes |
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| 1–18 Hz L(g) attenuation in the Granada Basin (southern Spain) |
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