Seismic noise tomography in regions with small velocity contrasts and strong noise directivity: application to the northern Baltic Shield

Ambient noise tomography (ANT) is widely used to image strong velocity variations within the upper crust . Using careful processing, we obtained a 3-D model of shear velocities in the upper crust beneath northern Finland, where the lateral velocity variations are less than 3%. As part of the tomogra...

Full description

Bibliographic Details
Main Authors: Poli, Piero, Campillo, M., Pedersen, Helle A.
Other Authors: Institut des Sciences de la Terre (ISTerre), Université Joseph Fourier - Grenoble 1 (UJF)-Institut Français des Sciences et Technologies des Transports, de l'Aménagement et des Réseaux (IFSTTAR)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de recherche pour le développement IRD : UR219-PRES Université de Grenoble-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)
Format: Report
Language:English
Published: HAL CCSD 2012
Subjects:
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Northern Finland
Lapland
Online Access:https://hal.science/hal-00721895
https://hal.science/hal-00721895/document
https://hal.science/hal-00721895/file/Complete_Manuscript.pdf
Description
Summary:Ambient noise tomography (ANT) is widely used to image strong velocity variations within the upper crust . Using careful processing, we obtained a 3-D model of shear velocities in the upper crust beneath northern Finland, where the lateral velocity variations are less than 3%. As part of the tomography, the noise field is analysed. It is strongly heterogeneous but the signal to noise ratio is sufficient to obtain stable dispersion curves for all profile azimuths. Our results show that the directions of dominant noise sources of Rayleigh and Love waves are the same, but the amplitude distribution with azimuth is different for the two types of waves. More intriguingly, the high frequency Love waves are dominated by a mixture of higher modes rather than the fundamental mode. The reconstructed 3-D model shows the Lapland Granulite Belt as a high velocity body with a limit at surface in excellent agreement with geological observations at surface. Following this interface at depth, our results are compatible with previous studies suggesting an archean north oriented subduction.

Similar Items