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...

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Bibliographic Details
Main Author: Barnes, Philip M.
Format: Article in Journal/Newspaper
Language:unknown
Published: University of Canterbury. Geology 1993
Subjects:
Online Access:https://dx.doi.org/10.26021/9065
https://ir.canterbury.ac.nz/handle/10092/4702