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Journal ArticleDOI

Structure of a growing accretionary prism, Hikurangi margin, New Zealand

TLDR
The Hikurangi margin of eastern North Island, New Zealand, represents the feather edge of the Indian plate at its convergent boundary with the subducting Pacific plate, and a migrated seismic reflection profile across this margin clearly displays the structural evolution of an accretionary prism as discussed by the authors.
Abstract
The Hikurangi margin of eastern North Island, New Zealand, represents the feather edge of the Indian plate at its convergent boundary with the subducting Pacific plate. A migrated seismic reflection profile across this margin clearly displays the structural evolution of an accretionary prism. A 25-km-wide band of “protothrusts” is delineated between the toe of the slope and a converging seamount; this illustrates an early stage in the seaward propagation of a deformation front. Landward-tilted trench-slope basins are separated by ridges that have clearly defined thrusts, which appear to sole out at a decollement. The decollement continues at an angle of only 3° beneath the 150-km-wide margin to a depth of 14 km near the coast where it coincides with an onshore zone of high seismicity.

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Spontaneous and triggered aseismic deformation transients in a subduction fault model

TL;DR: In this paper, the authors show that if interstitial fluids are present and pore pressure is near-lithostatic around and downdip from the frictional stability transition, transients with recurrence intervals of ∼1 year are predicted on the basis of laboratory friction parameters and their temperature (hence depth) variations.
Journal ArticleDOI

Tectonic and geological framework for gas hydrates and cold seeps on the Hikurangi subduction margin, New Zealand

TL;DR: In this paper, the authors identify approximately the contact between an inner foundation of deforming Late Cretaceous and Paleogene rocks, in which widespread out-of-sequence thrusting occurs, and a 65-70 km-wide outer wedge of late Cenozoic accreted turbidites.
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Geochemical Evolution within the Tonga–Kermadec–Lau Arc–Back-arc Systems: the Role of Varying Mantle Wedge Composition in Space and Time

TL;DR: In this article, trace element and isotope data for the active Tonga-Kermadec arc in the southwest Pacific, the volcano of Niua fo'ou in the back-arc Lau Basin, and Pacific Ocean sediments from DSDP Sites 204 and 275, and ODP Site 596, are integrated with existing geochemical data for lavas from the Lau basin, Samoa, the Louisville Ridge Seamount Chain (LR-SMC) and the extinct Lau Ridge arc, giving new insights into the petrogenesis of lavas in an active arc - back-
Journal ArticleDOI

Isotopic composition of helium, and CO2 and CH4 contents in gases produced along the New Zealand part of a convergent plate boundary

TL;DR: In this article, chemical and He isotopic analyses of 140 samples from all over New Zealand were performed to identify four major environments for mantle degassing: (1) areas of andesitic and rhyolitic volcanism and high-temperature geothermal activity over the center of the North Island, where 3He4He ratios approach typical crustal values of <0.1 RA.

Ambient Noise Rayleigh Wave Tomography of New Zealand

TL;DR: In this article, the authors present the first New Zealand-wide study of surface wave dispersion, using ambient noise observed at 42 broad-band stations in the national seismic network (GeoNet) and the Global Seismic Network (GSN).
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