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dc.creatorHaines, A. J.
dc.date1984-06-30
dc.date.accessioned2021-02-02T02:29:09Z
dc.date.available2021-02-02T02:29:09Z
dc.identifierhttps://bulletin.nzsee.org.nz/index.php/bnzsee/article/view/897
dc.identifier10.5459/bnzsee.17.2.145-153
dc.identifier.urihttps://repo.nzsee.org.nz/xmlui/handle/nzsee/1800
dc.descriptionA computer package has been developed to predict the pattern of SH-wave amplitudes in the vicinity of an earthquake. The phase-front parabolic approximation, which can be applied where there are significant lateral variations in the elastic constants within the Earth, has been adapted so that it also allows for surface topography. Examples are presented from a study of shaking in the Hutt Valley and the surrounding region as a result of movement on the Wellington Fault.en-US
dc.formatapplication/pdf
dc.languageeng
dc.publisherNew Zealand Society for Earthquake Engineeringen-US
dc.relationhttps://bulletin.nzsee.org.nz/index.php/bnzsee/article/view/897/872
dc.rightsCopyright (c) 1984 A. J. Hainesen-US
dc.rightshttps://creativecommons.org/licenses/by/4.0en-US
dc.sourceBulletin of the New Zealand Society for Earthquake Engineering; Vol 17 No 2 (1984); 145-153en-US
dc.source2324-1543
dc.source1174-9857
dc.titlePrediction of seismic wave amplitudes using the phase-front parabolic approximationen-US
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeArticleen-US


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