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New Zealand Journal of Geology and Geophysics abstracts


Refined slip distribution and moment magnitude of the 1848 Marlborough earthquake, Awatere Fault, New Zealand

Dougal P. M. Mason*
Timothy A. Little

School of Earth Sciences
Victoria University of Wellington
PO Box 600
Wellington, New Zealand
Dougal.Mason@opus.co.nz

*Present address: Opus International Consultants Ltd, PO Box 12003, Wellington, New Zealand.

Abstract  The Awatere Fault is an important element of the obliquely convergent plate boundary zone in northeastern South Island, New Zealand, and is comprised of two geomorphically distinct sections that join across a complex fault junction in the upper Awatere Valley. The Mw c. 7.5 Marlborough earthquake of 1848 ruptured a c. 110 km length of the eastern section of the Awatere Fault, from the South Island’s east coast extending inland to at least Barefell Pass. This study attempts to document the coseismic slip distribution during the 1848 earthquake rupture. We examine a previously unmapped length of the fault trace in the upper Awatere Valley, along which we measured as many small (metre-scale) geomorphic displacements as possible. Based on these new data, and previous observations of inferred 1848 slip on other parts of the Awatere Fault, we infer that the 1848 earthquake had a mean coseismic displacement of 5.3 ± 1.6 m, a surface rupture length of 100–110 km, and a moment magnitude of Mw = 7.4–7.7. This new moment magnitude estimate supports previous estimates based on regressions of geometrical rupture parameters inferred for the 1848 earthquake and attenuation models of felt intensities. The set of second-smallest horizontal geomorphic displacements (c. 8–15 m) are approximately double those attributed to the 1848 earthquake, suggesting the penultimate event was of a similar magnitude to the 1848 earthquake.

Keywords  1848 earthquake; Awatere Fault; earthquake magnitude; Marlborough; New Zealand; paleoseismology; strike-slip faults; South Island

G05041; Received 16 August 2005; accepted 9 June 2006; Online publication date 8 August 2006
New Zealand Journal of Geology & Geophysics, 2006, Vol. 49: 375–382
0028–8306/06/4903–0375  © The Royal Society of New Zealand 2006

PDF file of entire paper: Print-quality (2470K) | screen-quality (964K)


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