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

dc.contributor.author	Summerhayes, Colin Peter
dc.date.accessioned	2011-05-05T02:42:53Z
dc.date.accessioned	2022-10-26T03:57:31Z
dc.date.available	2011-05-05T02:42:53Z
dc.date.available	2022-10-26T03:57:31Z
dc.date.copyright	1966
dc.date.issued	1966
dc.identifier.uri	https://ir.wgtn.ac.nz/handle/123456789/24238
dc.description.abstract	The 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.format	pdf	en_NZ
dc.language	en_NZ
dc.language.iso	en_NZ
dc.publisher	Te Herenga Waka—Victoria University of Wellington	en_NZ
dc.title	'Bathymetry, geology, sediments and structure of the New Zealand subantarctic sea-floor'	en_NZ
dc.type	Text	en_NZ
vuwschema.type.vuw	Awarded Research Masters Thesis	en_NZ
thesis.degree.grantor	Te Herenga Waka—Victoria University of Wellington	en_NZ
thesis.degree.level	Masters	en_NZ

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