dc.contributor.author |
Lienert, Barry Ronald |
|
dc.date.accessioned |
2011-08-25T21:15:53Z |
|
dc.date.accessioned |
2022-10-30T18:48:57Z |
|
dc.date.available |
2011-08-25T21:15:53Z |
|
dc.date.available |
2022-10-30T18:48:57Z |
|
dc.date.copyright |
1971 |
|
dc.date.issued |
1971 |
|
dc.identifier.uri |
https://ir.wgtn.ac.nz/handle/123456789/25909 |
|
dc.description.abstract |
This thesis describes the instrumentation developed for measuring the low intensities of magnetisation found in sedimentary rocks. A spinner magnetometer has been constructed employing a coil-galvanometer amplifier detection system, and later, a fluxgate system.
The instrument has been used to determine the magnetic polarities of samples taken throughout 1000 metres of Pliocene-Miocene sedimentary strata at Hinakura Road, Wairarapa. These polarities have been correlated with accepted magnetic stratigraphies to yield a date for the Miocene-Pliocene boundary in New Zealand of 4.8 M yrs. |
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 |
Construction of a spinner magnetometer and paleomagnetic measurements on a Pliocenemiocene sedimentary section |
en_NZ |
dc.type |
Text |
en_NZ |
vuwschema.type.vuw |
Awarded Research Masters Thesis |
en_NZ |
thesis.degree.discipline |
Physics |
en_NZ |
thesis.degree.grantor |
Te Herenga Waka—Victoria University of Wellington |
en_NZ |
thesis.degree.level |
Masters |
en_NZ |