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'Bathymetry, geology, sediments and structure of the New Zealand subantarctic sea-floor'

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dc.contributor.authorSummerhayes, Colin Peter
dc.date.accessioned2011-05-05T02:42:53Z
dc.date.accessioned2022-10-26T03:57:31Z
dc.date.available2011-05-05T02:42:53Z
dc.date.available2022-10-26T03:57:31Z
dc.date.copyright1966
dc.date.issued1966
dc.description.abstractThe area considered in this work (Fig. I ) is that covered by N.Z.O.I. Campbell, Pukaki, Auckland and Macquarie charts (folder). It covers some 500,000 sq. miles between latitudes 48° and 57°30,S and longitudes 157° and 180°E. Bathymetric surveys of the seafloor south of New Zealand, show the normally abrupt transition from continental shelf to deep sea floor to be replaced by a broad marginal plateau in intermediate depths. The surrounding deep seafloor is also diversified by a major ridge-trough system.en_NZ
dc.formatpdfen_NZ
dc.identifier.urihttps://ir.wgtn.ac.nz/handle/123456789/24238
dc.languageen_NZ
dc.language.isoen_NZ
dc.publisherTe Herenga Waka—Victoria University of Wellingtonen_NZ
dc.rights.holderAll rights, except those explicitly waived, are held by the Authoren_NZ
dc.rights.licenseAuthor Retains Copyrighten_NZ
dc.rights.urihttps://www.wgtn.ac.nz/library/about-us/policies-and-strategies/copyright-for-the-researcharchive
dc.subjectMarine sedimentsen_NZ
dc.subjectOcean bottomen_NZ
dc.subjectSubmarine geologyen_NZ
dc.title'Bathymetry, geology, sediments and structure of the New Zealand subantarctic sea-floor'en_NZ
dc.typeTexten_NZ
thesis.degree.disciplineGeologyen_NZ
thesis.degree.grantorTe Herenga Waka—Victoria University of Wellingtonen_NZ
thesis.degree.levelMastersen_NZ
thesis.degree.nameMaster of Scienceen_NZ
vuwschema.type.vuwAwarded Research Masters Thesisen_NZ

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