Abstract
The intermediate depth seismicity of the northern part of the South Island has been found in the past to extend to a maximum depth of about 230 km. On 1990 Jun 22, an event occurred which was routinely located at a depth of 348 km in this region. Subsequently, a data search revealed another event in 1988 of similar depth and location, less well determined but acceptable. Both events have a magnitude ML = 3.4–3.5. In the future, consideration of the deep structure in this region should take into account the possible extension of seismicity to greater depths.
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