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dc.contributor.authorJupp, PE
dc.contributor.authorGoudie, IBJ
dc.contributor.authorBatchelor, RA
dc.contributor.authorGoudie, RJB
dc.date.accessioned2022-04-19T13:16:45Z
dc.date.available2022-04-19T13:16:45Z
dc.date.issued2022
dc.date.submitted2020-04-04
dc.identifier.issn0035-9254
dc.identifier.otherrssc12553
dc.identifier.urihttps://www.repository.cam.ac.uk/handle/1810/336151
dc.description.abstractSome planes in sedimentary rocks contain features that appear to lie near equally-spaced parallel lines. Determining whether or not they do so can provide information on possible mechanisms for their formation. The problem is recast here in terms of circular statistics, enabling closeness of candidate sets of lines to the points to be measured by a mean resultant length. This leads to a test of goodness of fit and to estimates of the direction of the lines and of the spacing between them. Two contrasting data sets are analysed.
dc.languageen
dc.publisherWiley
dc.subjectORIGINAL ARTICLE
dc.subjectORIGINAL ARTICLES
dc.subjectdirectional statistics
dc.subjectquantal model
dc.titleAssessing seismic origin of geological features by fitting equidistant parallel lines
dc.typeArticle
dc.date.updated2022-04-19T13:16:45Z
prism.publicationNameJournal of the Royal Statistical Society. Series C: Applied Statistics
dc.identifier.doi10.17863/CAM.83576
dcterms.dateAccepted2022-02-04
rioxxterms.versionofrecord10.1111/rssc.12553
rioxxterms.versionAO
rioxxterms.versionVoR
rioxxterms.licenseref.urihttp://creativecommons.org/licenses/by/4.0/
dc.contributor.orcidJupp, PE [0000-0003-0973-8434]
dc.contributor.orcidGoudie, IBJ [0000-0002-3910-7310]
dc.contributor.orcidGoudie, RJB [0000-0001-9554-1499]
dc.identifier.eissn1467-9876
pubs.funder-project-idMRC (unknown)
cam.issuedOnline2022-04-17


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