The structure and seismicity of Icelandic rifts
Three-fi fths of the Earth’s crust has been built at oceanic spreading centres in the last 160 million years. To explore crustal extension processes and the architecture of these constructive plate boundaries I have studied the oceanic rift in Iceland. Here the Mid Atlantic Ridge is anomalously elev...
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ftucambridgeesc:oai:eprints.esc.cam.ac.uk:3883 2023-05-15T16:46:21+02:00 The structure and seismicity of Icelandic rifts Green, Robert G. 2016-03 text image http://eprints.esc.cam.ac.uk/3883/ http://eprints.esc.cam.ac.uk/3883/1/Green_PhDthesis.pdf http://eprints.esc.cam.ac.uk/3883/2/Rob%20green%20cover.jpg en eng http://eprints.esc.cam.ac.uk/3883/1/Green_PhDthesis.pdf http://eprints.esc.cam.ac.uk/3883/2/Rob%20green%20cover.jpg Green, Robert G. (2016) The structure and seismicity of Icelandic rifts. PhD thesis, University of Cambridge. 02 - Geodynamics Geophysics and Tectonics Thesis NonPeerReviewed 2016 ftucambridgeesc 2020-08-27T18:09:49Z Three-fi fths of the Earth’s crust has been built at oceanic spreading centres in the last 160 million years. To explore crustal extension processes and the architecture of these constructive plate boundaries I have studied the oceanic rift in Iceland. Here the Mid Atlantic Ridge is anomalously elevated above sea level and thus easier to instrument. I have deployed and operated a dense network of seismometers in the remote volcanic highlands in central Iceland, and used the passive seismic data collected from this network to explore crustal structure and volcanic processes in the extensional rift zones. Thesis Iceland University of Cambridge, Department of Earth Sciences: ESC Publications Mid-Atlantic Ridge |
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Open Polar |
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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 Green, Robert G. The structure and seismicity of Icelandic rifts |
topic_facet |
02 - Geodynamics Geophysics and Tectonics |
description |
Three-fi fths of the Earth’s crust has been built at oceanic spreading centres in the last 160 million years. To explore crustal extension processes and the architecture of these constructive plate boundaries I have studied the oceanic rift in Iceland. Here the Mid Atlantic Ridge is anomalously elevated above sea level and thus easier to instrument. I have deployed and operated a dense network of seismometers in the remote volcanic highlands in central Iceland, and used the passive seismic data collected from this network to explore crustal structure and volcanic processes in the extensional rift zones. |
format |
Thesis |
author |
Green, Robert G. |
author_facet |
Green, Robert G. |
author_sort |
Green, Robert G. |
title |
The structure and seismicity of Icelandic rifts |
title_short |
The structure and seismicity of Icelandic rifts |
title_full |
The structure and seismicity of Icelandic rifts |
title_fullStr |
The structure and seismicity of Icelandic rifts |
title_full_unstemmed |
The structure and seismicity of Icelandic rifts |
title_sort |
structure and seismicity of icelandic rifts |
publishDate |
2016 |
url |
http://eprints.esc.cam.ac.uk/3883/ http://eprints.esc.cam.ac.uk/3883/1/Green_PhDthesis.pdf http://eprints.esc.cam.ac.uk/3883/2/Rob%20green%20cover.jpg |
geographic |
Mid-Atlantic Ridge |
geographic_facet |
Mid-Atlantic Ridge |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
http://eprints.esc.cam.ac.uk/3883/1/Green_PhDthesis.pdf http://eprints.esc.cam.ac.uk/3883/2/Rob%20green%20cover.jpg Green, Robert G. (2016) The structure and seismicity of Icelandic rifts. PhD thesis, University of Cambridge. |
_version_ |
1766036451188801536 |