The nature of Earth's correlation wavefield: late coda of large earthquakes

The seismic correlation wavefield constructed from the stacked cross-correlograms of the late coda of earthquake signals at stations across the globe provides a wealth of observed pulses as a function of inter-station distance. The interval from 3 to 10 h after the onset of major earthquakes is empl...

Full description

Bibliographic Details
Published in:Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences
Main Authors: Kennett, Brian, Pham, Thanh-Son
Format: Article in Journal/Newspaper
Language:English
Published: Royal Society of London
Subjects:
Online Access:http://hdl.handle.net/1885/255800
https://doi.org/10.1098/rspa.2018.0082
https://openresearch-repository.anu.edu.au/bitstream/1885/255800/3/01_Kennett_The_nature_of_Earth%2527s_2018.pdf.jpg
id ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/255800
record_format openpolar
spelling ftanucanberra:oai:openresearch-repository.anu.edu.au:1885/255800 2024-01-14T10:10:38+01:00 The nature of Earth's correlation wavefield: late coda of large earthquakes Kennett, Brian Pham, Thanh-Son application/pdf http://hdl.handle.net/1885/255800 https://doi.org/10.1098/rspa.2018.0082 https://openresearch-repository.anu.edu.au/bitstream/1885/255800/3/01_Kennett_The_nature_of_Earth%2527s_2018.pdf.jpg en_AU eng Royal Society of London 1364-5021 http://hdl.handle.net/1885/255800 doi:10.1098/rspa.2018.0082 https://openresearch-repository.anu.edu.au/bitstream/1885/255800/3/01_Kennett_The_nature_of_Earth%2527s_2018.pdf.jpg © 2018 The Author(s) Published by the Royal Society Proceedings of the Royal Society of London Series A: Mathematical, Physical and Engineering Sciences seismology correlation wavefield earthquake coda body waves Journal article ftanucanberra https://doi.org/10.1098/rspa.2018.0082 2023-12-15T09:35:16Z The seismic correlation wavefield constructed from the stacked cross-correlograms of the late coda of earthquake signals at stations across the globe provides a wealth of observed pulses as a function of inter-station distance. The interval from 3 to 10 h after the onset of major earthquakes is employed for the period range from 15 to 50 s. The observations can be well matched by synthetic seismograms for a radially stratified Earth. Many of the correlation phases have similar time behaviour to those in the regular wavefield, but others have no correspondence. All such correlation phases can be explained by the interaction of arrivals with a common slowness at the each of the stations being correlated. Using a generalized ray description of the seismic wavefield, the time-distance behaviour of these correlation phases arises from differences in accumulated phase on different propagation paths through the Earth. Distinct arrivals emerge from the correlation field when there are many ways in which combinations of seismic phases can arise with the same difference in propagation legs. The constituents of the late coda are dominated by steeply travelling waves, and in consequence features associated with multiple passages through the whole Earth emerge distinctly, such as high-order multiples of PKIKP. IRIS Data Services are funded through the Seismological Facilities for the Advancement of Geoscience and EarthScope (SAGE) Proposal of the National Science Foundation under Cooperative Agreement No. EAR1261681. T.S.P. is supported by an ANU PhD Scholarship Article in Journal/Newspaper Seismological Facilities for the Advancement of Geoscience and EarthScope Australian National University: ANU Digital Collections Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences 474 2214 20180082
institution Open Polar
collection Australian National University: ANU Digital Collections
op_collection_id ftanucanberra
language English
topic seismology
correlation wavefield
earthquake coda
body waves
spellingShingle seismology
correlation wavefield
earthquake coda
body waves
Kennett, Brian
Pham, Thanh-Son
The nature of Earth's correlation wavefield: late coda of large earthquakes
topic_facet seismology
correlation wavefield
earthquake coda
body waves
description The seismic correlation wavefield constructed from the stacked cross-correlograms of the late coda of earthquake signals at stations across the globe provides a wealth of observed pulses as a function of inter-station distance. The interval from 3 to 10 h after the onset of major earthquakes is employed for the period range from 15 to 50 s. The observations can be well matched by synthetic seismograms for a radially stratified Earth. Many of the correlation phases have similar time behaviour to those in the regular wavefield, but others have no correspondence. All such correlation phases can be explained by the interaction of arrivals with a common slowness at the each of the stations being correlated. Using a generalized ray description of the seismic wavefield, the time-distance behaviour of these correlation phases arises from differences in accumulated phase on different propagation paths through the Earth. Distinct arrivals emerge from the correlation field when there are many ways in which combinations of seismic phases can arise with the same difference in propagation legs. The constituents of the late coda are dominated by steeply travelling waves, and in consequence features associated with multiple passages through the whole Earth emerge distinctly, such as high-order multiples of PKIKP. IRIS Data Services are funded through the Seismological Facilities for the Advancement of Geoscience and EarthScope (SAGE) Proposal of the National Science Foundation under Cooperative Agreement No. EAR1261681. T.S.P. is supported by an ANU PhD Scholarship
format Article in Journal/Newspaper
author Kennett, Brian
Pham, Thanh-Son
author_facet Kennett, Brian
Pham, Thanh-Son
author_sort Kennett, Brian
title The nature of Earth's correlation wavefield: late coda of large earthquakes
title_short The nature of Earth's correlation wavefield: late coda of large earthquakes
title_full The nature of Earth's correlation wavefield: late coda of large earthquakes
title_fullStr The nature of Earth's correlation wavefield: late coda of large earthquakes
title_full_unstemmed The nature of Earth's correlation wavefield: late coda of large earthquakes
title_sort nature of earth's correlation wavefield: late coda of large earthquakes
publisher Royal Society of London
url http://hdl.handle.net/1885/255800
https://doi.org/10.1098/rspa.2018.0082
https://openresearch-repository.anu.edu.au/bitstream/1885/255800/3/01_Kennett_The_nature_of_Earth%2527s_2018.pdf.jpg
genre Seismological Facilities for the Advancement of Geoscience and EarthScope
genre_facet Seismological Facilities for the Advancement of Geoscience and EarthScope
op_source Proceedings of the Royal Society of London Series A: Mathematical, Physical and Engineering Sciences
op_relation 1364-5021
http://hdl.handle.net/1885/255800
doi:10.1098/rspa.2018.0082
https://openresearch-repository.anu.edu.au/bitstream/1885/255800/3/01_Kennett_The_nature_of_Earth%2527s_2018.pdf.jpg
op_rights © 2018 The Author(s) Published by the Royal Society
op_doi https://doi.org/10.1098/rspa.2018.0082
container_title Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences
container_volume 474
container_issue 2214
container_start_page 20180082
_version_ 1788065425677877248