4.2 Article

Strike-slip ground-surface rupture (Greendale Fault) associated with the 4 September 2010 Darfield earthquake, Canterbury, New Zealand

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Publisher

GEOLOGICAL SOC PUBL HOUSE
DOI: 10.1144/1470-9236/11-034

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Funding

  1. Earthquake Commission
  2. Foundation for Research, Science and Technology (now Ministry of Science and Innovation) through the New Zealand Natural Hazards Research Platform
  3. Geological Map of New Zealand

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This paper provides a photographic tour of the ground-surface rupture features of the Greendale Fault, formed during the 4 September 2010 Darfield earthquake. The fault, previously unknown, produced at least 29.5 km of strike-slip surface deformation of right-lateral (dextral) sense. Deformation, spread over a zone between 30 and 300 m wide, consisted mostly of horizontal flexure with subsidiary discrete shears, the latter only prominent where overall displacement across the zone exceeded about 1.5 m. A remarkable feature of this event was its location in an intensively farmed landscape, where a multitude of straight markers, such as fences, roads and ditches, allowed precise measurements of offsets, and permitted well-defined limits to be placed on the length and widths of the surface rupture deformation.

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