New Zealand falls on the edge of
both the Australian and Pacific tectonic plates, which are two of the major plate tectonics. Subduction occurs as result of the North Island of New Zealand which is located in the Pacific place pushing towards the Australian Plate. The Australian Plate is being subjected under the Pacific Plate as well because the two plates underneath Fiordland are moving towards each other in south of New Zealand. The Alpine fault is also found running across almost the whole length of New Zealand. This makes major earthquakes very prone in New Zealand while being on a transform boundary.

Resources
"Tectonic Setting of New Zealand: Astride a Plate Boundary Which Includes the Alpine Fault, Alpine Fault, Department of Geology, University of Otago, New Zealand." Tectonic Setting of New Zealand: Astride a Plate Boundary Which Includes the Alpine Fault, Alpine Fault, Department of Geology, University of Otago, New Zealand. N.p., n.d. Web. 14 Feb. 2016.
"Plate Collision in NZ." / Earthquakes at a Plate Boundary / Earthquakes / Science Topics / Learning / Home. N.p., n.d. Web. 14 Feb. 2016.