Tracking high-frequency seismic source evolution: 2004 Mw 8.1 Macquarie event

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dc.contributor.authorKennett, Brian
dc.contributor.authorGorbatov, Alexei
dc.contributor.authorSpiliopoulos, S.
dc.date.accessioned2015-12-10T22:40:32Z
dc.date.issued2014
dc.date.updated2015-12-09T10:59:55Z
dc.description.abstractThe 2004 Mw 8.1 event on 23 December 2004 near the Macquarie Ridge is a very large intraplate event that has been overshadowed by the M w 9.3 Sumatra-Andaman event only 3 days later. We are able to track the progress of source evolution by estimating the
dc.identifier.issn0094-8276
dc.identifier.urihttp://hdl.handle.net/1885/57496
dc.publisherAmerican Geophysical Union
dc.sourceGeophysical Research Letters
dc.titleTracking high-frequency seismic source evolution: 2004 Mw 8.1 Macquarie event
dc.typeJournal article
local.bibliographicCitation.issue4
local.bibliographicCitation.lastpage1193
local.bibliographicCitation.startpage1187
local.contributor.affiliationKennett, Brian, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationGorbatov, Alexei, Geoscience Australia
local.contributor.affiliationSpiliopoulos, S., Geoscience Australia
local.contributor.authoruidKennett, Brian, u8413736
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040407 - Seismology and Seismic Exploration
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationu4027924xPUB403
local.identifier.citationvolume41
local.identifier.doi10.1002/2013GL058935
local.identifier.scopusID2-s2.0-84894239831
local.type.statusPublished Version

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