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New Zealand Journal of Geology and Geophysics abstracts


Combining geomorphic observations with in situ cosmogenic isotope measurements to study anticline growth and fault propagation in Central Otago, New Zealand

Eleanor Bennett1
John Youngson2
James Jackson1*
Richard Norris2
Grant Raisbeck3
Françoise Yiou3

1Bullard Laboratories
Madingley Road
Cambridge CB3 0EZ, United Kingdom

2Department of Geology
University of Otago
P.O. Box 56
Dunedin, New Zealand

3Centre de Spectrométrie Nucléaire et de Spectrométrie
de Masse
IN2P3-CNRS
Bâtiment 108, 91405 Orsay, France

*Corresponding author: jackson@esc.cam.ac.uk

Abstract  Measurements of 10Be concentrations in quartz-rich boulders exposed by the uplift of anticlinal ranges in Central Otago, New Zealand, are used to investigate the fault propagation styles and rates for the underlying blind reverse faults. 10Be ages along Little Rough Ridge reveal the propagation rate for this fault to be between zero (i.e., not propagating at all, if the ages reflect emergence of a fault of fixed length through a sloping surface) and a maximum of 8.1 mm/yr, if the ages reflect true lateral growth. Regardless of the propagation rate, Little Rough Ridge has established its length rapidly compared with the rate at which it has accumulated displacement. On Raggedy Range, the 10Be ages, together with structural data, imply that the ridge reached its current length by the merging of several small fault segments. This study emphasises the importance of combining 10Be measurements with geomorphic observations. Without understanding the geomorphological context, 10Be exposure ages are difficult to interpret at all; but even with geomorphic data, the interpretation of these ages can still be ambiguous.

Keywords  fault propagation; 10Be; dating; drainage evolution; wind gaps; neotectonics

G05022; Received 16 May 2005; accepted 9 February 2006; Online publication date 12 May 2006
New Zealand Journal of Geology & Geophysics, 2006, Vol. 49: 217–231
0028–8306/06/4902–0217  © The Royal Society of New Zealand 2006

PDF file of entire paper: Print-quality (5511K) | screen-quality (1971K)


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