Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions

Teleseismic P-wave receiver functions (PRFs) in ice-covered regions are contaminated by reverberations within the ice-sheet. The crustal conversion events which are commonly used for identifying lithospheric structure are concealed by these ice reverberations. The problematic ice-phase reverberation...

Full description

Bibliographic Details
Main Authors: Dale Harpley, Steve Hearn, Shaun Strong
Format: Conference Object
Language:English
Published: Zenodo 2021
Subjects:
Online Access:https://doi.org/10.5281/zenodo.6586203
id ftzenodo:oai:zenodo.org:6586203
record_format openpolar
spelling ftzenodo:oai:zenodo.org:6586203 2024-09-15T17:48:25+00:00 Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions Dale Harpley Steve Hearn Shaun Strong 2021-09-15 https://doi.org/10.5281/zenodo.6586203 eng eng Zenodo https://zenodo.org/communities/aseg_extended_abstracts_2021 https://doi.org/10.5281/zenodo.6586202 https://doi.org/10.5281/zenodo.6586203 oai:zenodo.org:6586203 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode Australian Society of Exploration Geophysicists Extended Abstracts, Volume 2021, 3rd Australasian Exploration Geoscience Conference, Brisbane, 2021, (2021-09-15) AEGC, Australasian Exploration Geoscience Conference, Brisbane, Australia, 15-17 September 2021 receiver function ice-sheet reverberations Wiener filtering predictive deconvolution info:eu-repo/semantics/conferencePaper 2021 ftzenodo https://doi.org/10.5281/zenodo.658620310.5281/zenodo.6586202 2024-07-26T19:16:07Z Teleseismic P-wave receiver functions (PRFs) in ice-covered regions are contaminated by reverberations within the ice-sheet. The crustal conversion events which are commonly used for identifying lithospheric structure are concealed by these ice reverberations. The problematic ice-phase reverberations can, however, be exploited. We describe a practical process, incorporating a simple generalised linear inversion (GLI) stage, which yields an ice-sheet model. The derived ice model can then be used to design a Wiener filter aimed at attenuating ice phases, and revealing crustal phases in the PRF. Although it is theoretically approximate, the Wiener approach appears robust. Synthetic trialling, using realistic models, is essential for understanding the limitations of the algorithm. The full process has been applied at ice-covered stations in Antarctica and Greenland. In each case, we have derived robust models for the ice, and have successfully extracted crustal Ps phases from the contaminated receiver functions. Open-Access Online Publication: March 03, 2023 Conference Object Antarc* Antarctica Greenland Ice Sheet Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic receiver function
ice-sheet reverberations
Wiener filtering
predictive deconvolution
spellingShingle receiver function
ice-sheet reverberations
Wiener filtering
predictive deconvolution
Dale Harpley
Steve Hearn
Shaun Strong
Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions
topic_facet receiver function
ice-sheet reverberations
Wiener filtering
predictive deconvolution
description Teleseismic P-wave receiver functions (PRFs) in ice-covered regions are contaminated by reverberations within the ice-sheet. The crustal conversion events which are commonly used for identifying lithospheric structure are concealed by these ice reverberations. The problematic ice-phase reverberations can, however, be exploited. We describe a practical process, incorporating a simple generalised linear inversion (GLI) stage, which yields an ice-sheet model. The derived ice model can then be used to design a Wiener filter aimed at attenuating ice phases, and revealing crustal phases in the PRF. Although it is theoretically approximate, the Wiener approach appears robust. Synthetic trialling, using realistic models, is essential for understanding the limitations of the algorithm. The full process has been applied at ice-covered stations in Antarctica and Greenland. In each case, we have derived robust models for the ice, and have successfully extracted crustal Ps phases from the contaminated receiver functions. Open-Access Online Publication: March 03, 2023
format Conference Object
author Dale Harpley
Steve Hearn
Shaun Strong
author_facet Dale Harpley
Steve Hearn
Shaun Strong
author_sort Dale Harpley
title Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions
title_short Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions
title_full Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions
title_fullStr Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions
title_full_unstemmed Attenuation of ice-sheet reverberations in teleseismic P-wave receiver functions
title_sort attenuation of ice-sheet reverberations in teleseismic p-wave receiver functions
publisher Zenodo
publishDate 2021
url https://doi.org/10.5281/zenodo.6586203
genre Antarc*
Antarctica
Greenland
Ice Sheet
genre_facet Antarc*
Antarctica
Greenland
Ice Sheet
op_source Australian Society of Exploration Geophysicists Extended Abstracts, Volume 2021, 3rd Australasian Exploration Geoscience Conference, Brisbane, 2021, (2021-09-15)
AEGC, Australasian Exploration Geoscience Conference, Brisbane, Australia, 15-17 September 2021
op_relation https://zenodo.org/communities/aseg_extended_abstracts_2021
https://doi.org/10.5281/zenodo.6586202
https://doi.org/10.5281/zenodo.6586203
oai:zenodo.org:6586203
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.658620310.5281/zenodo.6586202
_version_ 1810289599691358208