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Australia's Moho: A test of the usefulness of gravity modelling for the determination of Moho depth

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Aitken, A R A; Salmon, Michelle; Kennett, Brian

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In general, seismic methods provide a reliable way to image the crust-mantle interface, which is marked by a rapid increase in seismic velocity (the Moho). However, the coverage provided by seismic networks is necessarily limited due to access difficultie

dc.contributor.authorAitken, A R A
dc.contributor.authorSalmon, Michelle
dc.contributor.authorKennett, Brian
dc.date.accessioned2015-12-13T23:02:10Z
dc.identifier.issn0040-1951
dc.identifier.urihttp://hdl.handle.net/1885/84765
dc.description.abstractIn general, seismic methods provide a reliable way to image the crust-mantle interface, which is marked by a rapid increase in seismic velocity (the Moho). However, the coverage provided by seismic networks is necessarily limited due to access difficultie
dc.publisherElsevier
dc.sourceTectonophysics
dc.titleAustralia's Moho: A test of the usefulness of gravity modelling for the determination of Moho depth
dc.typeJournal article
local.description.notesImported from ARIES
local.identifier.citationvolume609
dc.date.issued2013
local.identifier.absfor040407 - Seismology and Seismic Exploration
local.identifier.absfor040405 - Gravimetrics
local.identifier.ariespublicationf5625xPUB13015
local.type.statusPublished Version
local.contributor.affiliationAitken, A R A, University of Western Australia
local.contributor.affiliationSalmon, Michelle, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationKennett, Brian, College of Physical and Mathematical Sciences, ANU
local.description.embargo2037-12-31
local.bibliographicCitation.startpage468
local.bibliographicCitation.lastpage479
local.identifier.doi10.1016/j.tecto.2012.06.049
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
dc.date.updated2015-12-12T07:45:23Z
local.identifier.scopusID2-s2.0-84889079009
local.identifier.thomsonID000330201000024
CollectionsANU Research Publications

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