Port Nicholson and the “Plough” mechanism in transcurrent faulting
- 1 February 1962
- journal article
- research article
- Published by Taylor & Francis in New Zealand Journal of Geology and Geophysics
- Vol. 5 (1) , 189-191
- https://doi.org/10.1080/00288306.1962.10420120
Abstract
Port Nicholson depression may have been formed because the dextral transcurrent Wellington Fault has a skewed surface.Keywords
This publication has 1 reference indexed in Scilit:
- Possible of Piercement structures, local unconformities, and secondary basins in the Eastern Geosyncline, New ZealandNew Zealand Journal of Geology and Geophysics, 1958