Structural styles and sedimentation at the southern termination of the Hikurangi subduction zone, offshore North Canterbury, New Zealand
In the northern region of South Island, New Zealand, a major tectonic transition occurs in the obliquely convergent Australia-Pacific plate boundary. The southern end of the Hikurangi subduction zone terminates against the Chatham Rise, a submerged continental plateau on the Pacific Plate, which is...
| Main Author: | |
|---|---|
| Language: | en |
| Published: |
University of Canterbury. Geology
2010
|
| Online Access: | http://hdl.handle.net/10092/4702 |