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Paleoseismicity of the Wellington Fault, Pahiatua segment


, : Paleoseismicity of the Wellington Fault, Pahiatua segment. Geological Society of New Zealand Miscellaneous Publication: Pages 28. 1990.



Accession: 018458380

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Related references

Van Dissen Russell J.; Berryman K.R.; Pettinga J.R.; Hill N.L., 1992: Paleoseismicity of the Wellington-Hutt Valley segment of the Wellington Fault, North Island, New Zealand. The Wellington Fault is one of the major active right-lateral strike-slip faults of the southern North Island and represents a significant seismic hazard to the greater Wellington region. Trench excavations across the fault in the Long Gully/Karor...

Langridge R.M.; Berryman K.R.; Van Dissen R.J., 2005: Defining the geometric segmentation and Holocene slip rate of the Wellington Fault, New Zealand; the Pahiatua section. The Wellington Fault is a major active, right lateral, strike-slip fault in southern North Island that can be divided into three distinct geometric sections based on changes in neotectonic character and structural complexities. These are, from sou...

Grapes Rodney, 1989: Paleoseismicity of the Wellington Fault. Bulletin of the New Zealand National Society for Earthquake Engineering 22(1): 12

Hanson Jude, 1994: Paleoseismicity on the Wellington Fault in western Hawkes Bay. Geological Society of New Zealand Miscellaneous Publication 80A: 79

Beanland Sarah; Berryman Kelvin R., 1991: Paleoseismicity studies of the Wellington Fault northeast of the Tararua Ranges. Preliminary results from a suite of trenches excavated across the Wellington Fault, west of Pahiatua, reveal apparently non-uniform earthquake recurrence intervals. Having reported the paleoearthquake dates at the Napier Conference (though having...

Begg, J.G.; Langridge, R.M.; Van Dissen, R.J.; Little, T.A., 2008: Wellington Fault; neotectonics and earthquake geology of the Wellington-Hutt Valley segment. This all-day fieldtrip encompasses visits to key localities along the Wellington-Hutt Valley Segment of the Wellington Fault including, especially, sites where recent investigations have yielded new insights into the fault's rupture history a...

Rhoades, D.A.; Van Dissen, R.J.; Langridge, R.M.; Little, T.A.; Ninis, D.; Smith, E.G.C.; Robinson, R., 2011: Re-evaluation of conditional probability of rupture of the Wellington-Hutt Valley segment of the Wellington Fault. New information on the activity of the Wellington-Hutt Valley segment of the Wellington Fault, New Zealand, has become available from geological and modelling studies undertaken in the last several years as part of the "It's Our Fault&qu...

Begg J.G.; Perrin N.D.; Van Dissen R.J., 1997: The Wellington-Hutt Valley segment of the Wellington Fault; including hazard, engineering and planning implications. The purpose of this trip is to look at the on-shore part of the Wellington-Hutt Valley segment of the Wellington fault and the younger sediments in the area, and to evaluate their significance in terms of the age of the fault, long term slip rates...

Van Dissen R.J.; Berryman K.R.; Pettinga J.R.; Hill N.L., 1990: Seismic hazard assessment of the Wellington-Hutt Valley segment of the Wellington Fault; recurrence interval and timing of most recent surface rupture. Pages (unpaginated 1990

Van Dissen R.J.; Begg J.G.; Robinson R., 2001: The Akatarawa Fault; a newly discovered active fault in the Wellington region, and implications for increased hazard on the Wellington Fault. The active Akatarawa fault extends northeastward for ca 18 km from its junction with the Wellington fault near the Whakatikei terraces area of Upper Hutt to its junction with the Moonshine and Otaki Forks faults at Cloustonville in the Akatarawa v...