On the Origin of Seismic Anisotropy in the Shallow Crust of the Northern Volcanic Zone, Iceland ...
AbstractThe Icelandic crust is a product of its unique tectonic setting, where the interaction of an ascending mantle plume and the Mid‐Atlantic Ridge has caused elevated mantle melting, with the melt accreted and cooled in the crust to form an oceanic plateau. We investigate the strength and orient...
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American Geophysical Union (AGU)
2022
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Online Access: | https://dx.doi.org/10.17863/cam.80606 https://www.repository.cam.ac.uk/handle/1810/333183 |
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ftdatacite:10.17863/cam.80606 2024-02-27T08:41:55+00:00 On the Origin of Seismic Anisotropy in the Shallow Crust of the Northern Volcanic Zone, Iceland ... Bacon, CA Johnson, JH White, RS Rawlinson, N 2022 https://dx.doi.org/10.17863/cam.80606 https://www.repository.cam.ac.uk/handle/1810/333183 en eng American Geophysical Union (AGU) seismic anisotropy Askja Iceland shear-wave splitting stress modeling article-journal ScholarlyArticle JournalArticle Article 2022 ftdatacite https://doi.org/10.17863/cam.80606 2024-02-01T15:02:53Z AbstractThe Icelandic crust is a product of its unique tectonic setting, where the interaction of an ascending mantle plume and the Mid‐Atlantic Ridge has caused elevated mantle melting, with the melt accreted and cooled in the crust to form an oceanic plateau. We investigate the strength and orientation of seismic anisotropy in the upper crust of the Northern Volcanic Zone using local earthquake shear‐wave splitting, with a view to understanding how the contemporary stress field may influence sub‐wavelength structure and processes. This is achieved using a data set comprising 50,000 earthquakes located in the top 10 km of the crust, recorded by up to 70 stations over a 9 year period. We find that anisotropy is largely confined to the top 3–4 km of the crust, with an average delay time of 0.10 ± 0.05 s, and an average orientation of the fast axis of anisotropy of N014°E ± 27°, which is perpendicular to the spreading direction of the Eurasian and North American plates (N106°E). These results are consistent ... Article in Journal/Newspaper Iceland DataCite Metadata Store (German National Library of Science and Technology) Askja ENVELOPE(-16.802,-16.802,65.042,65.042) Mid-Atlantic Ridge |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
seismic anisotropy Askja Iceland shear-wave splitting stress modeling |
spellingShingle |
seismic anisotropy Askja Iceland shear-wave splitting stress modeling Bacon, CA Johnson, JH White, RS Rawlinson, N On the Origin of Seismic Anisotropy in the Shallow Crust of the Northern Volcanic Zone, Iceland ... |
topic_facet |
seismic anisotropy Askja Iceland shear-wave splitting stress modeling |
description |
AbstractThe Icelandic crust is a product of its unique tectonic setting, where the interaction of an ascending mantle plume and the Mid‐Atlantic Ridge has caused elevated mantle melting, with the melt accreted and cooled in the crust to form an oceanic plateau. We investigate the strength and orientation of seismic anisotropy in the upper crust of the Northern Volcanic Zone using local earthquake shear‐wave splitting, with a view to understanding how the contemporary stress field may influence sub‐wavelength structure and processes. This is achieved using a data set comprising 50,000 earthquakes located in the top 10 km of the crust, recorded by up to 70 stations over a 9 year period. We find that anisotropy is largely confined to the top 3–4 km of the crust, with an average delay time of 0.10 ± 0.05 s, and an average orientation of the fast axis of anisotropy of N014°E ± 27°, which is perpendicular to the spreading direction of the Eurasian and North American plates (N106°E). These results are consistent ... |
format |
Article in Journal/Newspaper |
author |
Bacon, CA Johnson, JH White, RS Rawlinson, N |
author_facet |
Bacon, CA Johnson, JH White, RS Rawlinson, N |
author_sort |
Bacon, CA |
title |
On the Origin of Seismic Anisotropy in the Shallow Crust of the Northern Volcanic Zone, Iceland ... |
title_short |
On the Origin of Seismic Anisotropy in the Shallow Crust of the Northern Volcanic Zone, Iceland ... |
title_full |
On the Origin of Seismic Anisotropy in the Shallow Crust of the Northern Volcanic Zone, Iceland ... |
title_fullStr |
On the Origin of Seismic Anisotropy in the Shallow Crust of the Northern Volcanic Zone, Iceland ... |
title_full_unstemmed |
On the Origin of Seismic Anisotropy in the Shallow Crust of the Northern Volcanic Zone, Iceland ... |
title_sort |
on the origin of seismic anisotropy in the shallow crust of the northern volcanic zone, iceland ... |
publisher |
American Geophysical Union (AGU) |
publishDate |
2022 |
url |
https://dx.doi.org/10.17863/cam.80606 https://www.repository.cam.ac.uk/handle/1810/333183 |
long_lat |
ENVELOPE(-16.802,-16.802,65.042,65.042) |
geographic |
Askja Mid-Atlantic Ridge |
geographic_facet |
Askja Mid-Atlantic Ridge |
genre |
Iceland |
genre_facet |
Iceland |
op_doi |
https://doi.org/10.17863/cam.80606 |
_version_ |
1792049266159517696 |