Marlborough Fault System

Marlborough Fault System
Map of the Marlborough Fault System
Major active fault zones of New Zealand showing variation in displacement vector of Pacific Plate relative to Australian Plate along the boundary

The Marlborough Fault System is a set of four large dextral strike-slip faults and other related structures in the northern part of South Island, New Zealand, which transfer displacement between the mainly transform plate boundary of the Alpine fault and the mainly destructive boundary of the Kermadec Trench, and together form the boundary between the Australian and Pacific Plates.[1]



The Marlborough Fault System consists of four main dominantly strike-slip fault strands, which together carry almost all of the displacement associated with the plate boundary. Other smaller faults form as splays of these main faults or accommodate deformation of the crust between them, such as the Newton and Hura Faults at the western end of the Hope Fault and the Jordan Thrust that formed the Seaward Kaikoura Range. The dextral strike-slip across this zone has also involved clockwise rotation of the intervening fault blocks of about 20° since the early Pliocene.[2]


The Marlborough Fault System formed at about 5 Ma, during the early Pliocene, in response to a change in plate motions. The new plate vector was significantly oblique to the Alpine Fault, causing an increased amount of convergence. The set of strike-slip faults formed to accommodate this change by taking up most of the strike-slip component. [3]


There are four main fault strands, although many other smaller faults, of either strike-slip or thrust type are known.

Hope Fault

The Hope Fault forms the southernmost part of the Marlborough Fault System. The estimated slip-rate during the Holocene is 20–25 mm/yr, just over half of the plate boundary displacement. At its northeastern end it links into the Jordan Thrust and most of the displacement is transferred onto that structure. It takes its name from the Hope River, which runs along one of the central fault segments.[1]

Clarence Fault

The Clarence Fault runs from close to the Alpine Fault to about 10 km west of Ward, where it appears to terminate abruptly. A Holocene slip-rate of 3.5–5.0 mm/yr is estimated for this fault. At the surface the displacement appears to be nearly pure horizontal, but continuous uplift of the neighbouring Inner Kaikoura Range over the same period, suggests that some of the dip-slip component thought to be present at depth on the fault zone is transferred onto thrust or reverse faults under the range.[4] An extra 10° of clockwise rotation has been recognised within the block that lies northeast of the tip of the Clarence fault.[2] It takes its name from the Clarence River, which follows the fault trace in the northeastern section of the fault.

Awatere Fault

It is formed of two main segments; the Molesworth section to the southwest and the Eastern section to the northeast. The estimated recent slip-rate for the Molesworth section is 4.4 mm/yr.[5] It takes its name from the Awatere River whose valley follows the fault trace along some of its length.

Wairau Fault

The Wairau Fault is sometimes regarded as a direct continuation of the Alpine Fault and may be referred to as the Alpine-Wairau Fault. It takes its name from the Wairau River, which follows the fault trace for most of its length. It has an estimated slip-rate of 3–5 mm/yr.[6]


All parts of the Marlborough Fault System are currently seismically active. Historical earthquakes (since European settlement) have occurred on both the Hope and Awatere Faults and on the smaller Poulter Fault. Studies of the geomorphology and the use of trenching across fault strands, has identified many earthquakes that occurred during the Holocene on many parts of the fault system.[1][4][5][6] The Hope Fault, which has the fastest slip rate is characterised by the shortest recurrence interval.


  1. ^ a b c Langridge, R.; Campbell J., Hill N., Pere V., Pope J., Pettinga J., Estrada B. & Berryman K. (2003). "Paleoseismology and slip rate of the Conway Segment of the Hope Fault at Greenburn Stream, South Island, New Zealand". Annals of Geophysics 46 (5). Retrieved 27 June 2010. 
  2. ^ a b Roberts, A.P. (1995). "Tectonic rotation about the termination of a major strike‐slip fault, Marlborough Fault System, New Zealand". Geophysical Research Letters 22 (3): 187–190. Bibcode 1995GeoRL..22..187R. doi:10.1029/94GL02582. Retrieved June 27, 2010. 
  3. ^ Musgrave, R.J.. "Early to Middle Miocene Pacific-Australia plate boundary in New Zealand: an alternative transcurrent-fault system". In Hillis R.R. & Müller R.D.. Evolution and dynamics of the Australian plate. Geological Society of Australia Special Publications. 22. Geological Society of America. pp. 333–341. ISBN 9780813723723. Retrieved 3 July 2010. 
  4. ^ a b Nicol, A.; Van Dissen R. (2002). "Up-dip partitioning of displacement components on the oblique-slip Clarence Fault, New Zealand". Journal of Structural Geology 24 (9): 1521–1535. doi:10.1016/S0191-8141(01)00141-9. 
  5. ^ a b Mason, D.P.M.; Little T.A. & Van Dissen R.J. (2006). "Rates of active faulting during late Quaternary fluvial terrace formation at Saxton River, Awatere fault, New Zealand". Geological Society of America Bulletin 118 (11-12): 1431–1446. doi:10.1130/B25961.1. Retrieved 27 June 2010. 
  6. ^ a b Zachariasen, J.; Berryman K., Langridge R., Prentice C., Rymer M., Striling M. & Villamor P. (2006). "Timing of late Holocene surface rupture of the Wairau Fault, Marlborough, New Zealand". New Zealand Journal of Geology and Geophysics 49 (1): 159–174. Retrieved 2 July 2010. 

Wikimedia Foundation. 2010.

Игры ⚽ Поможем решить контрольную работу

Look at other dictionaries:

  • North Island Fault System — Major active fault zones of New Zealand showing variation in displacement vector of Pacific Plate relative to Australian Plate along the boundary …   Wikipedia

  • Clarence Fault — Map of the Marlborough Fault System The Clarence Fault is an active dextral (right lateral) strike slip fault in the northeastern part of South Island, New Zealand. It forms part of the Marlborough Fault System, which accommodates the transfer of …   Wikipedia

  • Christchurch Fault — The Christchurch Fault is an active seismic fault running under the city of Christchurch in the middle of New Zealand s South Island. It runs from an area close to Riccarton, under the Central City, through the eastern suburbs off the coast of… …   Wikipedia

  • 2010 Canterbury earthquake — For the severe aftershock of 22 February 2011, see 2011 Christchurch earthquake. 2010 Canterbury earthquake …   Wikipedia

  • Geology of New Zealand — The continent of Zealandia The geology of New Zealand is noted for its volcanic activity, earthquakes and geothermal areas because of its position on the boundary of the Australian Plate and Pacific Plates. New Zealand was earlier part of the… …   Wikipedia

  • Earthquakes in New Zealand — Major active fault zones of New Zealand showing variation in displacement vector of Pacific Plate relative to Australian Plate along the boundary …   Wikipedia

  • Землетрясение в Крайстчёрче (2010) — О повторных сейсмических толчках 22 февраля 2011 см. Землетрясение в Крайстчёрче (2011). Землетрясение в Крайстчёрче 2010 года …   Википедия

  • Система разломов Марлборо — Карта системы разломов Марлборо …   Википедия

  • Alpine-Verwerfung — Die Alpine Fault, durch den Kontrast zwischen schneebedeckten Bergen und grüner Küstenebene in der oberen Bildhälfte klar als gerade Linie sichtbar, verläuft vom Westende der Southern Alps bis zur Nordostspitze von South Island …   Deutsch Wikipedia

  • 2011 Christchurch earthquake — Christchurch earthquake redirects here. For other uses, see Christchurch earthquake (disambiguation). For the 13 June 2011 aftershock, see June 2011 Christchurch earthquake. February 2011 Christchurch earthquake ChristChurch Cathedral and the… …   Wikipedia

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”