The south-west extension of the Awatere Fault
- 1 August 1961
- journal article
- research article
- Published by Taylor & Francis in New Zealand Journal of Geology and Geophysics
- Vol. 4 (3) , 264-269
- https://doi.org/10.1080/00288306.1961.10423126
Abstract
The Awatere Fault has been traced south-west to join the Alpine Fault at the Clear Grey River. The metamorphic zone boundaries of the Alpine schists are displaced dextrally by about four miles, but the Alpine Fault is not displaced.Keywords
This publication has 3 references indexed in Scilit:
- The tectonic history of New ZealandNew Zealand Journal of Geology and Geophysics, 1959
- Rationalized fault interpretationNew Zealand Journal of Geology and Geophysics, 1958
- Note on fault correlations across cook straitNew Zealand Journal of Geology and Geophysics, 1958