Opportune detections of global P-wave propagation from microseisms interferometry
Global seismological observations are sensitive to oceanic forcings, namely microseisms. In addition to dominant surface waves, these sources generate body waves that travel through the deep structures of our planet. Despite these sources’ inherent complexity, interferometric methods allow isolating...
Saved in:
Main Authors: | Boué, Pierre, Tomasetto, Lisa |
---|---|
Format: | Article |
Language: | English |
Published: |
Académie des sciences
2023-06-01
|
Series: | Comptes Rendus. Géoscience |
Subjects: | |
Online Access: | https://comptes-rendus.academie-sciences.fr/geoscience/articles/10.5802/crgeos.222/ |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Similar Items
-
Seismic wave propagation in stratified media /
by: Kennett, B. L. N.
Published: (1983) -
Dynamic of seismic noise sources in the Mediterranean Sea: implication for monitoring using noise correlations
by: Stehly, Laurent, et al.
Published: (2024-05-01) -
Determination of the structure of the earth's crust by changing the velocity of seismic waves from the earthquake data
by: B. I. Shakhtarin, et al.
Published: (2021-01-01) -
Seismic wave velocity in the New Guinea / Solomon Islands region
by: Brooks, J. A.
Published: (1963) -
Optical interferometry /
by: Hariharan, P.
Published: (1985)