Vertical Motions at the Fringes of the Icelandic Plume ...

The Icelandic mantle plume has had a profound influence on the development of the North Atlantic region over its 64 Myr existence. Long-wavelength free-air gravity anomalies and full waveform tomographic studies suggest that the planform of the plume is highly irregular, with up to five fingers of h...

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Main Author: Schoonman, Charlotte Maria
Format: Thesis
Language:English
Published: Apollo - University of Cambridge Repository 2017
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.13879
https://www.repository.cam.ac.uk/handle/1810/267950
id ftdatacite:10.17863/cam.13879
record_format openpolar
spelling ftdatacite:10.17863/cam.13879 2024-09-15T18:13:22+00:00 Vertical Motions at the Fringes of the Icelandic Plume ... Schoonman, Charlotte Maria 2017 https://dx.doi.org/10.17863/cam.13879 https://www.repository.cam.ac.uk/handle/1810/267950 en eng Apollo - University of Cambridge Repository open.access All Rights Reserved https://www.rioxx.net/licenses/all-rights-reserved/ http://purl.org/coar/access_right/c_abf2 geophysics seismology geodynamics mantle plumes Iceland British Isles dynamic topography receiver functions Scandinavia viscous fingering Dissertation thesis Thesis 2017 ftdatacite https://doi.org/10.17863/cam.13879 2024-07-03T13:13:19Z The Icelandic mantle plume has had a profound influence on the development of the North Atlantic region over its 64 Myr existence. Long-wavelength free-air gravity anomalies and full waveform tomographic studies suggest that the planform of the plume is highly irregular, with up to five fingers of hot asthenosphere radiating away from Iceland beneath the lithospheric plates. Two of these fingers extend beneath the British Isles and southern Scandinavia, where departures from crustal isostatic equilibrium and anomalous uplift have been identified. In this study, the spatial extent of present-day dynamic support associated with the Icelandic plume is investigated using receiver function analysis. Teleseismic events recorded at nine temporary and 59 permanent broadband, three-component seismometer stations are used to calculate 3864 P-to-S crustal receiver functions. The amplitude and arrival time of particular converted phases are assessed, and H-$\textit{k}$ stacking is applied to estimate bulk crustal ... Thesis Iceland North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic geophysics
seismology
geodynamics
mantle plumes
Iceland
British Isles
dynamic topography
receiver functions
Scandinavia
viscous fingering
spellingShingle geophysics
seismology
geodynamics
mantle plumes
Iceland
British Isles
dynamic topography
receiver functions
Scandinavia
viscous fingering
Schoonman, Charlotte Maria
Vertical Motions at the Fringes of the Icelandic Plume ...
topic_facet geophysics
seismology
geodynamics
mantle plumes
Iceland
British Isles
dynamic topography
receiver functions
Scandinavia
viscous fingering
description The Icelandic mantle plume has had a profound influence on the development of the North Atlantic region over its 64 Myr existence. Long-wavelength free-air gravity anomalies and full waveform tomographic studies suggest that the planform of the plume is highly irregular, with up to five fingers of hot asthenosphere radiating away from Iceland beneath the lithospheric plates. Two of these fingers extend beneath the British Isles and southern Scandinavia, where departures from crustal isostatic equilibrium and anomalous uplift have been identified. In this study, the spatial extent of present-day dynamic support associated with the Icelandic plume is investigated using receiver function analysis. Teleseismic events recorded at nine temporary and 59 permanent broadband, three-component seismometer stations are used to calculate 3864 P-to-S crustal receiver functions. The amplitude and arrival time of particular converted phases are assessed, and H-$\textit{k}$ stacking is applied to estimate bulk crustal ...
format Thesis
author Schoonman, Charlotte Maria
author_facet Schoonman, Charlotte Maria
author_sort Schoonman, Charlotte Maria
title Vertical Motions at the Fringes of the Icelandic Plume ...
title_short Vertical Motions at the Fringes of the Icelandic Plume ...
title_full Vertical Motions at the Fringes of the Icelandic Plume ...
title_fullStr Vertical Motions at the Fringes of the Icelandic Plume ...
title_full_unstemmed Vertical Motions at the Fringes of the Icelandic Plume ...
title_sort vertical motions at the fringes of the icelandic plume ...
publisher Apollo - University of Cambridge Repository
publishDate 2017
url https://dx.doi.org/10.17863/cam.13879
https://www.repository.cam.ac.uk/handle/1810/267950
genre Iceland
North Atlantic
genre_facet Iceland
North Atlantic
op_rights open.access
All Rights Reserved
https://www.rioxx.net/licenses/all-rights-reserved/
http://purl.org/coar/access_right/c_abf2
op_doi https://doi.org/10.17863/cam.13879
_version_ 1810451128110809088