Crustal structure of Iceland and Greenland from receiver function studies
We used data from both permanent and temporary seismic networks on Iceland and Greenland to investigate the crustal thickness by partly reinterpreting earlier data (P receiver functions) and adding S receiver functions to better constrain the results. We obtained good conversions from the Moho and a...
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Online Access: | http://eprints.esc.cam.ac.uk/461/ http://eprints.esc.cam.ac.uk/461/1/Priestley_JGR_112_2007.pdf https://doi.org/10.1029/2005JB003991 |
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ftucambridgeesc:oai:eprints.esc.cam.ac.uk:461 2023-05-15T16:23:53+02:00 Crustal structure of Iceland and Greenland from receiver function studies Kumar, P. Kind, R. Priestley, K. F. Dahl-Jensen, T. 2007 application/pdf http://eprints.esc.cam.ac.uk/461/ http://eprints.esc.cam.ac.uk/461/1/Priestley_JGR_112_2007.pdf https://doi.org/10.1029/2005JB003991 en eng http://eprints.esc.cam.ac.uk/461/1/Priestley_JGR_112_2007.pdf Kumar, P. and Kind, R. and Priestley, K. F. and Dahl-Jensen, T. (2007) Crustal structure of Iceland and Greenland from receiver function studies. Journal of Geophysical Research, 112, (B3). B03301. DOI https://doi.org/10.1029/2005JB003991 <https://doi.org/10.1029/2005JB003991> 02 - Geodynamics Geophysics and Tectonics Article PeerReviewed 2007 ftucambridgeesc https://doi.org/10.1029/2005JB003991 2020-08-27T18:08:32Z We used data from both permanent and temporary seismic networks on Iceland and Greenland to investigate the crustal thickness by partly reinterpreting earlier data (P receiver functions) and adding S receiver functions to better constrain the results. We obtained good conversions from the Moho and also crustal multiples in both Iceland and Greenland. The central ice covered part of Greenland has an average crustal thickness of 40 km, typical for a craton. At the edges of Greenland the crustal thickness decreases to 30–40 km. On the east coast of Greenland, where the track of the Iceland plume is thought to have affected the lithosphere, the crustal thickness is only 24–26 km. In contrast to previous studies, we find that the crustal thickness in the east and the northwest coastal regions of Iceland is more than 40 km, similar to beneath the active volcanic region. In the southwest region of Iceland and along the mid-ocean ridge, the crustal thickness is only 25 km or less. Also in contrast to earlier receiver function interpretations, which deduced a broad crust-mantle transition zone for Iceland, we find indications for a normal, sharper Moho beneath a number of sites. Article in Journal/Newspaper Greenland Iceland University of Cambridge, Department of Earth Sciences: ESC Publications Greenland Journal of Geophysical Research 112 B3 |
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Open Polar |
collection |
University of Cambridge, Department of Earth Sciences: ESC Publications |
op_collection_id |
ftucambridgeesc |
language |
English |
topic |
02 - Geodynamics Geophysics and Tectonics |
spellingShingle |
02 - Geodynamics Geophysics and Tectonics Kumar, P. Kind, R. Priestley, K. F. Dahl-Jensen, T. Crustal structure of Iceland and Greenland from receiver function studies |
topic_facet |
02 - Geodynamics Geophysics and Tectonics |
description |
We used data from both permanent and temporary seismic networks on Iceland and Greenland to investigate the crustal thickness by partly reinterpreting earlier data (P receiver functions) and adding S receiver functions to better constrain the results. We obtained good conversions from the Moho and also crustal multiples in both Iceland and Greenland. The central ice covered part of Greenland has an average crustal thickness of 40 km, typical for a craton. At the edges of Greenland the crustal thickness decreases to 30–40 km. On the east coast of Greenland, where the track of the Iceland plume is thought to have affected the lithosphere, the crustal thickness is only 24–26 km. In contrast to previous studies, we find that the crustal thickness in the east and the northwest coastal regions of Iceland is more than 40 km, similar to beneath the active volcanic region. In the southwest region of Iceland and along the mid-ocean ridge, the crustal thickness is only 25 km or less. Also in contrast to earlier receiver function interpretations, which deduced a broad crust-mantle transition zone for Iceland, we find indications for a normal, sharper Moho beneath a number of sites. |
format |
Article in Journal/Newspaper |
author |
Kumar, P. Kind, R. Priestley, K. F. Dahl-Jensen, T. |
author_facet |
Kumar, P. Kind, R. Priestley, K. F. Dahl-Jensen, T. |
author_sort |
Kumar, P. |
title |
Crustal structure of Iceland and Greenland from receiver function studies |
title_short |
Crustal structure of Iceland and Greenland from receiver function studies |
title_full |
Crustal structure of Iceland and Greenland from receiver function studies |
title_fullStr |
Crustal structure of Iceland and Greenland from receiver function studies |
title_full_unstemmed |
Crustal structure of Iceland and Greenland from receiver function studies |
title_sort |
crustal structure of iceland and greenland from receiver function studies |
publishDate |
2007 |
url |
http://eprints.esc.cam.ac.uk/461/ http://eprints.esc.cam.ac.uk/461/1/Priestley_JGR_112_2007.pdf https://doi.org/10.1029/2005JB003991 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Iceland |
genre_facet |
Greenland Iceland |
op_relation |
http://eprints.esc.cam.ac.uk/461/1/Priestley_JGR_112_2007.pdf Kumar, P. and Kind, R. and Priestley, K. F. and Dahl-Jensen, T. (2007) Crustal structure of Iceland and Greenland from receiver function studies. Journal of Geophysical Research, 112, (B3). B03301. DOI https://doi.org/10.1029/2005JB003991 <https://doi.org/10.1029/2005JB003991> |
op_doi |
https://doi.org/10.1029/2005JB003991 |
container_title |
Journal of Geophysical Research |
container_volume |
112 |
container_issue |
B3 |
_version_ |
1766012230634045440 |