Marlborough fault system

Marlborough fault system
Marlborough tectonic domain
Map of the Marlborough fault system
EtymologyMarlborough
CountryNew Zealand
RegionMarlborough
Characteristics
DisplacementTotal strike-slip across system is up to 48 mm (1.9 in)/year.[1]
Tectonics
PlateIndo-Australian, Pacific
StatusActive
Earthquakes7.8 Mw 2016 Kaikōura earthquake[2]
TypeStrike-slip faults
MovementDextral/convergent, east side up
AgeAlbian-Meghalayan 105–0 Ma[2]
OrogenyKaikōura
New Zealand geology database (includes faults)
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 (also known as Marlborough tectonic domain[2]) 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.[3]

  1. ^ Khajavi, Narges; Nicol, Andrew; Quigley, Mark C.; Langridge, Robert M. (2018). "Temporal slip-rate stability and variations on the Hope Fault, New Zealand, during the late Quaternary". Tectonophysics. 738–739: 112–123. Bibcode:2018Tectp.738..112K. doi:10.1016/j.tecto.2018.05.001. ISSN 0040-1951. S2CID 135144626.
  2. ^ a b c Berryman, K.; Rattenbury, M.; Bannister, S.; Ellis, S.; Villamor, P.; Eberhart-Phillips, D.O.; Upton, P.; Howell, A. (2023). "Geological structure informs rupture propagation and surface rupture complexity during the 2016 Kaikōura earthquake, New Zealand: insights for future large earthquake hazard". Turkish Journal of Earth Sciences. 32 (3): 330–50. doi:10.55730/1300-0985.1848.
  3. ^ Cite error: The named reference Langridge was invoked but never defined (see the help page).