Please use this identifier to cite or link to this item: https://superindex.lbr.auckland.ac.nz/handle/123456789/65365
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dc.creatorHampton, Samuel Job-
dc.date.accessioned2013-05-31T01:53:29Z-
dc.date.available2013-05-31T01:53:29Z-
dc.date.issued2010-
dc.identifier.urihttp://hdl.handle.net/123456789/65365-
dc.description.abstractThe Lyttelton Volcanic Complex, north-western Banks Peninsula, New Zealand, is comprised of five overlapping volcanic cones. Two magma systems are postulated to have fed Banks Peninsula��_s basaltic intraplate volcanism, with simultaneous volcanism occurring in both the north-western and south-eastern regions of Banks Peninsula, to form Lyttelton and Akaroa Volcanic Complexes respectively-
dc.description.sponsorshipCU-
dc.relation.urihttp://ir.canterbury.ac.nz/handle/10092/4117-
dc.subjectGeomorphology-
dc.subjectVolcanology-
dc.titleGrowth, structure and evolution the Lyttelton Volcanic Complex, Banks Peninsula, New Zealand-
thesis.degree.levelPhD-
thesis.degree.grantorUniversity of Canterbury-
dcterms.spatialLyttelton-
dcterms.spatialBanks Peninsula-
dcterms.spatialLyttelton Volcano-
dcterms.spatialAkaroa-
dc.subject.keywordsintraplate process-
dc.subject.keywordseruption-
dc.subject.keywordsbasaltic composition-
Appears in Collections:Earth Science Theses

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