Now showing items 1-2 of 2
Morphostructural and paleo-seismic analysis of fault interactions in the Oxford–Cust–Ashley fault system, Canterbury
(University of Canterbury. Geological Sciences, 2015)
This study investigates evidence for linkages and fault interactions centred on the Cust Anticline in Northwest Canterbury between Starvation Hill to the southwest and the Ashley and Loburn faults to the northeast. An ...
Modelling Submarine Landscape Evolution in Response to Subduction Processes, Northern Hikurangi Margin, New Zealand
(University of Canterbury. Geological Sciences, 2010)
The steep forearc slope along the northern sector of the obliquely convergent Hikurangi subduction zone is characteristic of non-accretionary and tectonically eroding continental margins, with reduced sediment supply in ...