Elastic and non-elastic surface deformation in New Zealand

  • G. J. Lensen New Zealand Geological Survey, Lower Hutt, New Zealand

Abstract

Over the last decade it has become evident that not all surface deformation takes place during earthquakes. Deformation associated with earthquakes and their aftershocks appears to be non-elastic in nature, while in between earthquakes deformation appears to be elastic.

References

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Published
1970-12-31
How to Cite
Lensen, G. J. (1970). Elastic and non-elastic surface deformation in New Zealand. Bulletin of the New Zealand Society for Earthquake Engineering, 3(4), 131-142. https://doi.org/10.5459/bnzsee.3.4.131-142
Section
Articles