Distribution of stress state in the Nankai subduction zone, southwest Japan and a comparison with Japan Trench

W Lin, TB Byrne, M Kinoshita, LC McNeill, C Chang… - Tectonophysics, 2016 - Elsevier
To better understand the distribution of three dimensional stress states in the Nankai
subduction zone, southwest Japan, we review various stress-related investigations carried …

Expedition 372B/375 summary

DM Saffer, LM Wallace, PM Barnes… - Proceedings of the …, 2019 - oceanrep.geomar.de
Slow slip events (SSEs) at the northern Hikurangi subduction margin, New Zealand, are
among the best-documented shallow SSEs on Earth. International Ocean Discovery …

Model test on the behavior of tunnel linings under earth pressure conditions and external water pressure

BG He, Y Zhang, ZQ Zhang, XT Feng, ZJ Sun - Transportation Geotechnics, 2021 - Elsevier
km long tunnels of major highways in Shanxi Province of China are observed, and 5120
crack distributions are obtained that are largely dependent on both earth pressure …

Characterization of hydrate and gas reservoirs in plate convergent margin by applying rock physics to high-resolution seismic velocity model

C Chhun, A Kioka, J Jia, T Tsuji - Marine and Petroleum Geology, 2018 - Elsevier
Gas hydrates are widely distributed in the Kumano forearc basin, which is located above
accretionary prism in the Nankai margin off the Kii peninsula, Japan. Bottom-Simulating …

Spatial variation of shallow stress orientation along the Hikurangi Subduction Margin: Insights from in‐situ borehole image logging

E Behboudi, DD McNamara, I Lokmer… - Journal of …, 2022 - Wiley Online Library
Abstract Knowledge of the contemporary in‐situ stress orientations in the Earth's crust can
improve our understanding of active crustal deformation, geodynamic processes, and …

In situ stress and pore pressure in the deep interior of the Nankai accretionary prism, integrated ocean drilling program site C0002

H Kitajima, D Saffer, H Sone, H Tobin… - Geophysical Research …, 2017 - Wiley Online Library
Strength and slip behaviors of subduction megathrusts are controlled by the physical
properties and stress state not only of the fault zones themselves but also the adjacent wall …

In situ stress magnitudes at the toe of the Nankai Trough Accretionary Prism, offshore Shikoku Island, Japan

KA Huffman, DM Saffer - Journal of Geophysical Research …, 2016 - Wiley Online Library
Quantifying the orientation and magnitude of tectonic stresses is essential toward
understanding deformation and faulting in subduction zones. However, constraints on in situ …

[HTML][HTML] Expedition 372B/375 methods

LM Wallace - Expedition, 2019 - publications.iodp.org
Site U1518 is located on the lower continental slope near the Hikurangi Trench
approximately 62 km from shore in~ 2630 m water depth. The site lies on the frontal …

Early sedimentation and deformation in the K umano forearc basin linked with N ankai accretionary prism evolution, southwest J apan

SG Ramirez, SPS Gulick… - Geochemistry …, 2015 - Wiley Online Library
Early forearc basin sedimentation and subsidence appear to be linked with convergent
margin evolution, yet they do not follow predictable spatiotemporal patterns. In the Kumano …

Direct constraints on in situ stress state from deep drilling into the Nankai subduction zone, Japan

HJ Tobin, DM Saffer, DA Castillo, T Hirose - Geology, 2022 - pubs.geoscienceworld.org
Stress state is a long-sought but poorly known parameter on subduction megathrusts and in
overlying accretionary wedges in general. We used direct observations made during drilling …