Seismic anisotropy and microseismicity: from crustal formation to subduction termination ...
The plate tectonic cycle is fundamental to our dynamic Earth, encompassing the formation and evolution of new lithosphere at divergent, mid-ocean ridges, all the way to its eventual return to, and re-equilibration with, the mantle in subduction zones. I investigate the structure of the crust and upp...
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ftdatacite:10.17863/cam.82196 2024-02-04T10:01:25+01:00 Seismic anisotropy and microseismicity: from crustal formation to subduction termination ... Bacon, Conor 2021 https://dx.doi.org/10.17863/cam.82196 https://www.repository.cam.ac.uk/handle/1810/334765 en eng Apollo - University of Cambridge Repository open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 seismic anisotropy seismology tectonics volcano seismology microseismicity Iceland Southeast Asia Dissertation Thesis thesis 2021 ftdatacite https://doi.org/10.17863/cam.82196 2024-01-05T14:56:35Z The plate tectonic cycle is fundamental to our dynamic Earth, encompassing the formation and evolution of new lithosphere at divergent, mid-ocean ridges, all the way to its eventual return to, and re-equilibration with, the mantle in subduction zones. I investigate the structure of the crust and upper mantle of the Earth in two regions that represent different endmembers in this cycle through the analysis of microseismicity and seismic anisotropy, seeking to learn more about the stresses in these environments and how they are manifest in the structure of the subsurface. In Iceland, new oceanic crust is accreted episodically within the volcanic rift zones that delineate the subaerial portion of the Mid-Atlantic Ridge, the divergent margin between the North American and the Eurasian plates. Northern Borneo, conversely, exhibits the tectonic signatures of not one but two terminated subduction zones, where oceanic lithosphere was once being actively recycled into the Earth’s mantle. As part of this work, I have ... Thesis Iceland DataCite Metadata Store (German National Library of Science and Technology) Mid-Atlantic Ridge |
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DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
seismic anisotropy seismology tectonics volcano seismology microseismicity Iceland Southeast Asia |
spellingShingle |
seismic anisotropy seismology tectonics volcano seismology microseismicity Iceland Southeast Asia Bacon, Conor Seismic anisotropy and microseismicity: from crustal formation to subduction termination ... |
topic_facet |
seismic anisotropy seismology tectonics volcano seismology microseismicity Iceland Southeast Asia |
description |
The plate tectonic cycle is fundamental to our dynamic Earth, encompassing the formation and evolution of new lithosphere at divergent, mid-ocean ridges, all the way to its eventual return to, and re-equilibration with, the mantle in subduction zones. I investigate the structure of the crust and upper mantle of the Earth in two regions that represent different endmembers in this cycle through the analysis of microseismicity and seismic anisotropy, seeking to learn more about the stresses in these environments and how they are manifest in the structure of the subsurface. In Iceland, new oceanic crust is accreted episodically within the volcanic rift zones that delineate the subaerial portion of the Mid-Atlantic Ridge, the divergent margin between the North American and the Eurasian plates. Northern Borneo, conversely, exhibits the tectonic signatures of not one but two terminated subduction zones, where oceanic lithosphere was once being actively recycled into the Earth’s mantle. As part of this work, I have ... |
format |
Thesis |
author |
Bacon, Conor |
author_facet |
Bacon, Conor |
author_sort |
Bacon, Conor |
title |
Seismic anisotropy and microseismicity: from crustal formation to subduction termination ... |
title_short |
Seismic anisotropy and microseismicity: from crustal formation to subduction termination ... |
title_full |
Seismic anisotropy and microseismicity: from crustal formation to subduction termination ... |
title_fullStr |
Seismic anisotropy and microseismicity: from crustal formation to subduction termination ... |
title_full_unstemmed |
Seismic anisotropy and microseismicity: from crustal formation to subduction termination ... |
title_sort |
seismic anisotropy and microseismicity: from crustal formation to subduction termination ... |
publisher |
Apollo - University of Cambridge Repository |
publishDate |
2021 |
url |
https://dx.doi.org/10.17863/cam.82196 https://www.repository.cam.ac.uk/handle/1810/334765 |
geographic |
Mid-Atlantic Ridge |
geographic_facet |
Mid-Atlantic Ridge |
genre |
Iceland |
genre_facet |
Iceland |
op_rights |
open.access Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.82196 |
_version_ |
1789967303501152256 |