A model of active faulting in New Zealand

被引：168

作者：

Litchfield, N. J. ^{[1
]}

Van Dissen, R. ^{[1
]}

Sutherland, R. ^{[1
]}

Barnes, P. M. ^{[2
]}

Cox, S. C. ^{[3
]}

Norris, R. ^{[4
]}

Beavan, R. J. ^{[1
]}

Langridge, R. ^{[1
]}

Villamor, P. ^{[1
]}

Berryman, K. ^{[1
]}

Stirling, M. ^{[1
]}

Nicol, A. ^{[1
]}

Nodder, S. ^{[2
]}

Lamarche, G. ^{[2
]}

Barrell, D. J. A. ^{[3
]}

Pettinga, J. R. ^{[5
]}

Little, T. ^{[6
]}

Pondard, N. ^{[1
]}

Mountjoy, J. J. ^{[2
]}

Clark, K. ^{[1
]}

机构：

[1] GNS Sci, Lower Hutt, New Zealand

[2] Natl Inst Water & Atmospher Res NIWA, Wellington, New Zealand

[3] GNS Sci, Dunedin, New Zealand

[4] Univ Otago, Dept Geol, Dunedin, New Zealand

[5] Univ Canterbury, Dept Geol Sci, Christchurch 1, New Zealand

[6] Victoria Univ Wellington, Sch Geog Environm & Earth Sci, Wellington, New Zealand

来源：

NEW ZEALAND JOURNAL OF GEOLOGY AND GEOPHYSICS | 2014年 / 57卷 / 01期

关键词：

active fault; New Zealand; tectonic domain; plate boundary; kinematics; slip rate; TAUPO VOLCANIC ZONE; DARFIELD CANTERBURY EARTHQUAKE; HIKURANGI SUBDUCTION ZONE; OFFSHORE ALPINE FAULT; SEISMIC HAZARD MODEL; QUATERNARY SLIP RATE; SOUTH-ISLAND; STRIKE-SLIP; NORTH CANTERBURY; PLATE BOUNDARY;

D O I：

10.1080/00288306.2013.854256

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

Active fault traces are a surface expression of permanent deformation that accommodates the motion within and between adjacent tectonic plates. We present an updated national-scale model for active faulting in New Zealand, summarize the current understanding of fault kinematics in 15 tectonic domains, and undertake some brief kinematic analysis including comparison of fault slip rates with GPS velocities. The model contains 635 simplified faults with tabulated parameters of their attitude (dip and dip-direction) and kinematics (sense of movement and rake of slip vector), net slip rate and a quality code. Fault density and slip rates are, as expected, highest along the central plate boundary zone, but the model is undoubtedly incomplete, particularly in rapidly eroding mountainous areas and submarine areas with limited data. The active fault data presented are of value to a range of kinematic, active fault and seismic hazard studies.

引用

页码：32 / 56

页数：25

共 196 条

[51] A comparison of historical and paleoseismicity in a newly formed fault zone and a mature fault zone, North Canterbury, New Zealand [J].