Basini et al., 2013 - Google Patents
The influence of nonuniform ambient noise on crustal tomography in EuropeBasini et al., 2013
View PDF- Document ID
- 17691511914917127970
- Author
- Basini P
- Nissen‐Meyer T
- Boschi L
- Casarotti E
- Verbeke J
- Schenk O
- Giardini D
- Publication year
- Publication venue
- Geochemistry, Geophysics, Geosystems
External Links
Snippet
Ambient‐noise seismology is of great relevance to high‐resolution crustal imaging, thanks to the unprecedented dense data coverage it affords in regions of little seismicity. Under the assumption of uniformly distributed noise sources, it has been used to extract the Green's …
- 238000003325 tomography 0 title abstract description 12
Classifications
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/28—Processing seismic data, e.g. analysis, for interpretation, for correction
- G01V1/30—Analysis
- G01V1/303—Analysis for determining velocity profiles or travel times
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/003—Seismic data acquisition in general, e.g. survey design
- G01V1/005—Seismic data acquisition in general, e.g. survey design with exploration systems emitting special signals, e.g. frequency swept signals, pulse sequences or slip sweep arrangements
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/28—Processing seismic data, e.g. analysis, for interpretation, for correction
- G01V1/282—Application of seismic models, synthetic seismograms
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/28—Processing seismic data, e.g. analysis, for interpretation, for correction
- G01V1/36—Effecting static or dynamic corrections on records, e.g. correcting spread; Correlating seismic signals; Eliminating effects of unwanted energy
- G01V1/364—Seismic filtering
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V2210/00—Details of seismic processing or analysis
- G01V2210/60—Analysis
- G01V2210/61—Analysis by combining or comparing a seismic data set with other data
- G01V2210/614—Synthetically generated data
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V2210/00—Details of seismic processing or analysis
- G01V2210/60—Analysis
- G01V2210/67—Wave propagation modeling
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/16—Receiving elements for seismic signals; Arrangements or adaptations of receiving elements
- G01V1/18—Receiving elements, e.g. seismometer, geophone or torque detectors, for localised single point measurements
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V2210/00—Details of seismic processing or analysis
- G01V2210/30—Noise handling
- G01V2210/32—Noise reduction
- G01V2210/322—Trace stacking
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V3/00—Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation
- G01V3/12—Electric or magnetic prospecting or detecting; Measuring magnetic field characteristics of the earth, e.g. declination, deviation operating with electromagnetic waves
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/008—Earthquake measurement or prediction
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/40—Seismology; Seismic or acoustic prospecting or detecting specially adapted for well-logging
- G01V1/42—Seismology; Seismic or acoustic prospecting or detecting specially adapted for well-logging using generators in one well and receivers elsewhere or vice versa
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V2210/00—Details of seismic processing or analysis
- G01V2210/50—Corrections or adjustments related to wave propagation
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V99/00—Subject matter not provided for in other groups of this subclass
- G01V99/005—Geomodels or geomodelling, not related to particular measurements
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS
- G01V11/00—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS prospecting or detecting by methods combining techniques covered by two or more of main groups G01V1/00 - G01V9/00
-
- G—PHYSICS
- G06—COMPUTING; CALCULATING; COUNTING
- G06F—ELECTRICAL DIGITAL DATA PROCESSING
- G06F17/00—Digital computing or data processing equipment or methods, specially adapted for specific functions
- G06F17/10—Complex mathematical operations
Similar Documents
| Publication | Publication Date | Title |
|---|---|---|
| Wang et al. | Frequency‐Bessel transform method for effective imaging of higher‐mode Rayleigh dispersion curves from ambient seismic noise data | |
| Thomas et al. | Spatiotemporal evolution of seismic and aseismic slip on the Longitudinal Valley Fault, Taiwan | |
| Fang et al. | A new algorithm for three‐dimensional joint inversion of body wave and surface wave data and its application to the Southern California plate boundary region | |
| Obermann et al. | Seismic noise correlations to image structural and mechanical changes associated with the Mw 7.9 2008 Wenchuan earthquake | |
| Dalton et al. | The global attenuation structure of the upper mantle | |
| Landès et al. | Origin of deep ocean microseisms by using teleseismic body waves | |
| Monteiller et al. | Three-dimensional full waveform inversion of short-period teleseismic wavefields based upon the SEM–DSM hybrid method | |
| Eberhart‐Phillips et al. | Three‐dimensional attenuation model of the shallow Hikurangi subduction zone in the Raukumara Peninsula, New Zealand | |
| Sager et al. | Global‐scale full‐waveform ambient noise inversion | |
| Basini et al. | The influence of nonuniform ambient noise on crustal tomography in Europe | |
| Li et al. | An effective method to extract overtones of surface wave from array seismic records of earthquake events | |
| Shang et al. | Beyond receiver functions: Passive source reverse time migration and inverse scattering of converted waves | |
| Silwal et al. | Seismic moment tensors and estimated uncertainties in southern Alaska | |
| Mordret et al. | Seismic noise‐based time‐lapse monitoring of the Valhall overburden | |
| Wang et al. | Urban basin structure imaging based on dense arrays and Bayesian array‐based coherent receiver functions | |
| Hillers et al. | Interaction of microseisms with crustal heterogeneity: A case study from the San Jacinto fault zone area | |
| Hannemann et al. | Three‐dimensional shallow structure from high‐frequency ambient noise tomography: New results for the Mygdonia basin‐Euroseistest area, northern Greece | |
| Jia et al. | Determination of near surface shear‐wave velocities in the central Los Angeles basin with dense arrays | |
| Mordret et al. | Azimuthal anisotropy at Valhall: The Helmholtz equation approach | |
| Sager et al. | Sensitivity of seismic noise correlation functions to global noise sources | |
| Luo et al. | Apparent low‐velocity belt in the shallow Anninghe fault zone in SW China and its implications for seismotectonics and earthquake hazard assessment | |
| Li et al. | Joint inversion of Rayleigh wave phase velocity, particle motion, and teleseismic body wave data for sedimentary structures | |
| Yue et al. | Validation of linearity assumptions for using tsunami waveforms in joint inversion of kinematic rupture models: Application to the 2010 Mentawai Mw 7.8 tsunami earthquake | |
| Godano et al. | Bayesian inversion of seismic spectral ratio for source scaling: Application to a persistent multiplet in the western Corinth rift | |
| Ajala et al. | Effect of merging multiscale models on seismic wavefield predictions near the southern San Andreas fault |