Décollement strength and mechanical segmentation along the frontal wedge of the Hikurangi convergent margin (New Zealand): Insights from critical taper analysis-Reference-Cited by-同舟云学术

Décollement strength and mechanical segmentation along the frontal wedge of the Hikurangi convergent margin (New Zealand): Insights from critical taper analysis

Published:2022-12 Issue: Volume:844 Page:229622
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Schwarze Cornelius O.,Kukowski Nina

Funder

Federal Ministry of Education and Research Bonn Office

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference91 articles.

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3. Evolution of the Upper Cenozoic Magmatic Arc and plate boundary in northern New Zealand;Ballance;Earth Planet. Sci. Lett.,1976

4. Geometry of the Hikurangi subduction thrust and upper plate, North Island, New Zealand;Barker;Geochem. Geophys. Geosyst.,2009

5. Rates and mechanics of rapid frontal accretion along the very obliquely convergent southern Hikurangi margin, New Zealand;Barnes;Journal of Geophysical Research: Solid Earth,1997

Cited by 2 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Accretion Cycles, Structural Evolution, and Thrust Activity in Accretionary Wedges With Various Décollement Configurations: Insights From Sandbox Analog Modeling;Journal of Geophysical Research: Solid Earth;2023-12

2. Geochemical and isotopic characterisation of trench sediment at the Hikurangi Margin from IODP sites U1518 and U1520;New Zealand Journal of Geology and Geophysics;2023-11-20