Noise directivity and group velocity tomography in a region with small velocity contrasts: 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 per cent. As part of the...
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2013
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fthighwire:oai:open-archive.highwire.org:gji:192/1/413 2023-05-15T17:42:31+02:00 Noise directivity and group velocity tomography in a region with small velocity contrasts: the northern Baltic shield Poli, P. Pedersen, H. A. Campillo;, M. the POLENET/LAPNET Working Group 2013-01-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/192/1/413 https://doi.org/10.1093/gji/ggs034 en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/192/1/413 http://dx.doi.org/10.1093/gji/ggs034 Copyright (C) 2013, Oxford University Press Seismology TEXT 2013 fthighwire https://doi.org/10.1093/gji/ggs034 2015-02-28T20:39:58Z 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 per cent. 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. Text Northern Finland Lapland HighWire Press (Stanford University) Geophysical Journal International 192 1 413 424 |
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Open Polar |
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HighWire Press (Stanford University) |
op_collection_id |
fthighwire |
language |
English |
topic |
Seismology |
spellingShingle |
Seismology Poli, P. Pedersen, H. A. Campillo;, M. the POLENET/LAPNET Working Group Noise directivity and group velocity tomography in a region with small velocity contrasts: the northern Baltic shield |
topic_facet |
Seismology |
description |
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 per cent. 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. |
format |
Text |
author |
Poli, P. Pedersen, H. A. Campillo;, M. the POLENET/LAPNET Working Group |
author_facet |
Poli, P. Pedersen, H. A. Campillo;, M. the POLENET/LAPNET Working Group |
author_sort |
Poli, P. |
title |
Noise directivity and group velocity tomography in a region with small velocity contrasts: the northern Baltic shield |
title_short |
Noise directivity and group velocity tomography in a region with small velocity contrasts: the northern Baltic shield |
title_full |
Noise directivity and group velocity tomography in a region with small velocity contrasts: the northern Baltic shield |
title_fullStr |
Noise directivity and group velocity tomography in a region with small velocity contrasts: the northern Baltic shield |
title_full_unstemmed |
Noise directivity and group velocity tomography in a region with small velocity contrasts: the northern Baltic shield |
title_sort |
noise directivity and group velocity tomography in a region with small velocity contrasts: the northern baltic shield |
publisher |
Oxford University Press |
publishDate |
2013 |
url |
http://gji.oxfordjournals.org/cgi/content/short/192/1/413 https://doi.org/10.1093/gji/ggs034 |
genre |
Northern Finland Lapland |
genre_facet |
Northern Finland Lapland |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/192/1/413 http://dx.doi.org/10.1093/gji/ggs034 |
op_rights |
Copyright (C) 2013, Oxford University Press |
op_doi |
https://doi.org/10.1093/gji/ggs034 |
container_title |
Geophysical Journal International |
container_volume |
192 |
container_issue |
1 |
container_start_page |
413 |
op_container_end_page |
424 |
_version_ |
1766144382663131136 |