Effects of the Iceland plume on Greenland's lithosphere: New insights from ambient noise tomography
Ambient noise tomography is used to image Greenland's lithosphere, which passed over the Iceland plume between ∼70 and ∼40 Ma. Cross-correlations from 21 stations from GLISN seismic network were used to invert for 2-D Rayleigh wave phase velocity maps for 14 periods between 8 and 40 s. We find...
Published in: | Polar Science |
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Main Authors: | , |
Language: | English |
Published: |
2018
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Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/records/15105 |
_version_ | 1829307698544377856 |
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author | Antonijevic, Sanja Knezevic Lees, Jonathan M. |
author_facet | Antonijevic, Sanja Knezevic Lees, Jonathan M. |
author_sort | Antonijevic, Sanja Knezevic |
collection | National Institute of Polar Research Repository, Japan |
container_start_page | 75 |
container_title | Polar Science |
container_volume | 17 |
description | Ambient noise tomography is used to image Greenland's lithosphere, which passed over the Iceland plume between ∼70 and ∼40 Ma. Cross-correlations from 21 stations from GLISN seismic network were used to invert for 2-D Rayleigh wave phase velocity maps for 14 periods between 8 and 40 s. We find that Rayleigh wave phase velocities substantially vary across Greenland, with slow velocities coinciding with NW-SE trending Iceland plume track. In east Greenland the detected velocity reduction at longer periods (33–40s) reflects substantially thinned lithosphere, thermally ablated by the plume. From the east, the reduced velocities shift NW at shorter periods (12–20s), indicating shallowing of the plume-related slow anomaly. In north-central Greenland, the reduced velocities appear in the proximity of the plume ∼60 Ma, reflecting lithospheric weakening in the presence of residual heat that still persists within the lithosphere. Our results provide important new constraints on variations in the seismic velocity structure of Greenland's crust and uppermost mantle, revealing prolonged effects of the mantle plume on the overpassing craton. journal article |
genre | East Greenland Greenland Iceland Polar Science Polar Science |
genre_facet | East Greenland Greenland Iceland Polar Science Polar Science |
geographic | Greenland |
geographic_facet | Greenland |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00015105 |
institution | Open Polar |
language | English |
op_collection_id | ftnipr |
op_container_end_page | 82 |
op_doi | https://doi.org/10.1016/j.polar.2018.06.004 |
op_relation | 10.1016/j.polar.2018.06.004 https://doi.org/10.1016/j.polar.2018.06.004 Polar Science 17 75 82 18739652 https://nipr.repo.nii.ac.jp/records/15105 |
op_rights | metadata only access |
publishDate | 2018 |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00015105 2025-04-13T14:18:03+00:00 Effects of the Iceland plume on Greenland's lithosphere: New insights from ambient noise tomography Antonijevic, Sanja Knezevic Lees, Jonathan M. 2018-09 https://nipr.repo.nii.ac.jp/records/15105 eng eng 10.1016/j.polar.2018.06.004 https://doi.org/10.1016/j.polar.2018.06.004 Polar Science 17 75 82 18739652 https://nipr.repo.nii.ac.jp/records/15105 metadata only access Greenland's lithosphere Iceland plume track Lithospheric thinning and weakening 2018 ftnipr https://doi.org/10.1016/j.polar.2018.06.004 2025-03-19T10:19:56Z Ambient noise tomography is used to image Greenland's lithosphere, which passed over the Iceland plume between ∼70 and ∼40 Ma. Cross-correlations from 21 stations from GLISN seismic network were used to invert for 2-D Rayleigh wave phase velocity maps for 14 periods between 8 and 40 s. We find that Rayleigh wave phase velocities substantially vary across Greenland, with slow velocities coinciding with NW-SE trending Iceland plume track. In east Greenland the detected velocity reduction at longer periods (33–40s) reflects substantially thinned lithosphere, thermally ablated by the plume. From the east, the reduced velocities shift NW at shorter periods (12–20s), indicating shallowing of the plume-related slow anomaly. In north-central Greenland, the reduced velocities appear in the proximity of the plume ∼60 Ma, reflecting lithospheric weakening in the presence of residual heat that still persists within the lithosphere. Our results provide important new constraints on variations in the seismic velocity structure of Greenland's crust and uppermost mantle, revealing prolonged effects of the mantle plume on the overpassing craton. journal article Other/Unknown Material East Greenland Greenland Iceland Polar Science Polar Science National Institute of Polar Research Repository, Japan Greenland Polar Science 17 75 82 |
spellingShingle | Greenland's lithosphere Iceland plume track Lithospheric thinning and weakening Antonijevic, Sanja Knezevic Lees, Jonathan M. Effects of the Iceland plume on Greenland's lithosphere: New insights from ambient noise tomography |
title | Effects of the Iceland plume on Greenland's lithosphere: New insights from ambient noise tomography |
title_full | Effects of the Iceland plume on Greenland's lithosphere: New insights from ambient noise tomography |
title_fullStr | Effects of the Iceland plume on Greenland's lithosphere: New insights from ambient noise tomography |
title_full_unstemmed | Effects of the Iceland plume on Greenland's lithosphere: New insights from ambient noise tomography |
title_short | Effects of the Iceland plume on Greenland's lithosphere: New insights from ambient noise tomography |
title_sort | effects of the iceland plume on greenland's lithosphere: new insights from ambient noise tomography |
topic | Greenland's lithosphere Iceland plume track Lithospheric thinning and weakening |
topic_facet | Greenland's lithosphere Iceland plume track Lithospheric thinning and weakening |
url | https://nipr.repo.nii.ac.jp/records/15105 |