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New Zealand Journal of Geology & Geophysics abstracts


Short communication

Reassessment of slip rate and implications for surface rupture hazard of the Martinborough Fault, South Wairarapa, New Zealand

Nicola Litchfield*

Russell Van Dissen

Andrew Nicol

GNS Science
PO Box 30368
Lower Hutt 5040, New Zealand

*Corresponding author: n.litchfield@gns.cri.nz

Abstract New mapping of the Martinborough Fault utilising high resolution LIDAR data and orthophotos defines a c. 1.3 km long active fold trace consisting of a broad (50–150 m wide) warp crossing dissected alluvial fans. GPS survey profiles across the fold-scarp reveal vertical separations ranging from 1.2 to 6 m on two fan surfaces. Published OSL ages imply a Porewan age for the upper fan (surface age c. 55 ka). We calculate a revised vertical slip rate of c. 0.1 mm/yr (previously published rates range between 0.3 and 0.67 mm/yr) and a recurrence interval of c. 15 000 yr from these new data. This places the fault within the Ministry for the Environment Active Fault Guidelines Recurrence Interval Class V (>10 000 to ≤20 000 yr), to which a medium level of confidence is assigned.

Keywords Martinborough Fault; Wairarapa; reverse fault; slip rate; alluvial fan; MfE Active Fault Guidelines

G07007; Online publication date 25 July 2007; Received 2 May 2007; accepted 28 June 2007

New Zealand Journal of Geology & Geophysics, 2007, Vol. 50: 239–243
0028–8306/07/5003–0239  © The Royal Society of New Zealand 2007

PDF file of entire paper: Print-quality (1997K) | screen-quality (733K)


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