1 / 12

Tracking the origin of the seismic noise

Tracking the origin of the seismic noise. Tracking the origin of the seismic noise. Tracking the origin of the seismic noise. Apparent origin of the noise. Average sea wave height. winter. summer. Importance of scattering: a simple laboratory experiment with a few sources. C(A,X).

hyatt-suarez
Download Presentation

Tracking the origin of the seismic noise

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Tracking the originof the seismic noise

  2. Tracking the originof the seismic noise

  3. Tracking the origin of the seismic noise

  4. Apparent origin of the noise Average sea wave height winter summer

  5. Importance of scattering: a simple laboratory experiment with a few sources C(A,X) Correlations in water G(A,X) travel time A Xs sources receivers Correlations in presence of scattering

  6. x3 x θ y n x1 ψ THE 2D SCALAR CASE H(2)n(kr)=Jn(kr) − iYn(kr) Illumination by plane waves Azimuthal average over ψ leads to SPAC method  k  C

  7. Keiiti Aki x3 x θ y n x1 ψ A isotropic distribution of plane waves in an homogeneous body : the local approach THE 2D SCALAR CASE SH waves in a homogeneous elastic medium Propagation takes place in the x1-x3 plane. Therefore, the antiplane (out-of-plane) displacement v(x,t) fulfils the wave equation where β = shear wave velocity and t = time. A typical harmonic, homogeneous plane wave can be written as where, F(ω, ψ) = complex waveform, ω=circular frequency, xT = (x1, x3) = Cartesian coordinates x1= r cosθ = , x3 = r sinθ = , with r,θ = polar coordinates nj = direction cosines (n1= cos ψ , n3 = sin ψ ) Consider the auto-correlation of the motion, evaluated at positions x and y, respectively. For simplicity assume y at the origin: .

  8. Cross-correlations of seismic noise: ANMO - CCM (from Shapiro and Campillo, GRL, 2004) 30 days of vertical motion Dispersion analysis global model by Ritzwoller et al. 2002

  9. correlations computed over four different three-week periods PHL - MLAC 290 km band- passed 15 - 30 s band- passed 5 - 10 s repetitive measurements provide uncertainty estimations

  10. t G/2 (Re) (Im, Re) t (Im) Causality

More Related