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dc.contributor.authorKamp, Peter J.J.en_US
dc.contributor.authorVonk, Adam J.en_US
dc.contributor.authorBland, Kyle J.en_US
dc.contributor.authorHansen, Rochelle J.en_US
dc.contributor.authorHendy, Austin J.W.en_US
dc.contributor.authorMcIntyre, Avon P.en_US
dc.contributor.authorNgatai, Melodieen_US
dc.contributor.authorCartwright, Stuart J.en_US
dc.contributor.authorHayton, Shaunen_US
dc.contributor.authorNelson, Campbell S.en_US
dc.date.accessioned2008-03-19T05:08:04Z
dc.date.available2007-04-23en_US
dc.date.available2008-03-19T05:08:04Z
dc.date.issued2004-12-01en_US
dc.identifier.citationKamp, P. J. J., et al. (2004). Neogene stratigraphic architecture and tectonic evolution of Wanganui, King Country, and eastern Taranaki Basins, New Zealand. New Zealand Journal of Geology & Geophysics. 47(4), 625-644.en_US
dc.identifier.urihttps://hdl.handle.net/10289/177
dc.description.abstractAnalysis of the stratigraphic architecture of the fills of Wanganui, King Country, and eastern Taranaki Basins reveals the occurrence of five 2nd order Late Paleocene and Neogene sequences of tectonic origin. The oldest is the late Eocene-Oligocene Te Kuiti Sequence, followed by the early-early Miocene (Otaian) Mahoenui Sequence, followed by the late-early Miocene (Altonian) Mokau Sequence, all three in King Country Basin. The fourth is the middle Miocene to early Pliocene Whangamomona Sequence, and the fifth is the middle Pliocene-Pleistocene Rangitikei Sequence, both represented in the three basins. Higher order sequences (4th, 5th, 6th) with a eustatic origin occur particularly within the Whangamomona and Rangitikei Sequences, particularly those of 6th order with 41 000 yr periodicity.en_US
dc.format.mimetypeapplication/pdf
dc.language.isoen
dc.publisherSIR Publishingen_NZ
dc.relation.urihttp://www.rsnz.org/publish/nzjgg/2004/047.phpen_US
dc.rightsThis article has been published in the New Zealand Journal of Geology and Geophysics. (c) 2004 Royal Society of New Zealand.en_US
dc.subjectNorth Islanden_US
dc.subjectWanganui Basinen_US
dc.subjectKing Country Basinen_US
dc.subjectTaranaki Basinen_US
dc.subjectTaranaki Faulten_US
dc.subjectPungapunga Formationen_US
dc.subjectWhangamomona Groupen_US
dc.subjectRangitikei Supergroupen_US
dc.subjectsequence stratigraphyen_US
dc.subjecttectonicsen_US
dc.subjectnew structural namesen_US
dc.subjectnew stratigraphic namesen_US
dc.titleNeogene stratigraphic architecture and tectonic evolution of Wanganui, King Country, and eastern Taranaki Basins, New Zealanden_US
dc.typeJournal Articleen_US
dc.identifier.doi10.1080/00288306.2004.9515080en_NZ
dc.relation.isPartOfNew Zealand Journal of Geology & Geophysicsen_NZ
pubs.begin-page625en_NZ
pubs.elements-id30428
pubs.end-page644en_NZ
pubs.issue4en_NZ
pubs.volume47en_NZ


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