Abstract
The 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
Link
http://ir.canterbury.ac.nz/handle/10092/4117
| Title | Growth, structure and evolution the Lyttelton Volcanic Complex, Banks Peninsula, New Zealand |
|---|---|
| Author | Hampton, Samuel Job |
| Date | 2010 |
| Degree Level | Doctor of Philosophy |
| Degree Grantor | University of Canterbury |
| Focus | Geomorphology; Volcanology |
| Keywords | intraplate process; eruption; basaltic composition |
| Locality | Lyttelton; Banks Peninsula; Lyttelton Volcano; Akaroa |