In situ stress state in the Nankai accretionary wedge estimated from borehole wall failures

C Chang, LC McNeill, JC Moore, W Lin… - Geochemistry …, 2010 - Wiley Online Library
We constrain the orientations and magnitudes of in situ stress tensors using borehole wall
failures (borehole breakouts and drilling‐induced tensile fractures) detected in four vertical …

[HTML][HTML] Pore pressure distribution of a mega-splay fault system in the Nankai Trough subduction zone: Insight into up-dip extent of the seismogenic zone

T Tsuji, R Kamei, RG Pratt - Earth and Planetary Science Letters, 2014 - Elsevier
We use the pore pressure distribution predicted from a waveform tomography (WT) velocity
model to interpret the evolution of the mega-splay fault system in the Nankai Trough off …

Direct assessment of the hydraulic structure of the plate boundary at the toe of the Nankai accretionary prism

J Pwavodi, ML Doan - Geophysical Journal International, 2024 - academic.oup.com
SUMMARY The Nankai Trough is a locus of slow slip, low-frequency earthquakes, and large
magnitude (M w> 8) earthquakes. It is usually assumed that high pore pressure contributes …

Slow wavespeeds and fluid overpressure in a region of shallow geodetic locking and slow slip, Hikurangi subduction margin, New Zealand

D Bassett, R Sutherland, S Henrys - Earth and Planetary Science Letters, 2014 - Elsevier
Travel times recorded onshore from active-source marine seismic surveys were used to
determine Hikurangi forearc wavespeeds. Ray-path midpoints sample forearc crust above …

Anelastic strain recovery reveals extension across SW Japan subduction zone

TB Byrne, W Lin, A Tsutsumi… - Geophysical …, 2009 - Wiley Online Library
Sediment dominated convergent margins typically record substantial horizontal shortening
often associated with great earthquakes. The convergent margin south of Japan is arguably …

Present‐day principal horizontal stress orientations in the Kumano forearc basin of the southwest Japan subduction zone determined from IODP NanTroSEIZE drilling …

W Lin, ML Doan, JC Moore, L McNeill… - Geophysical …, 2010 - Wiley Online Library
A 1.6 km riser borehole was drilled at site C0009 of the NanTroSEIZE, in the center of the
Kumano forearc basin, as a landward extension of previous drilling in the southwest Japan …

Expedition 349 summary

CF Li, J Lin, DK Kulhanek, T Williams, R Bao, A Briais… - 2015 - boris.unibe.ch
C.-F. Li, J. Lin, DK Kulhanek, T. Williams, R. Bao, A. Briais, EA Brown, Y. Chen, PD Clift, FS
Colwell, KA Dadd, W.-W. Ding, I. Hernández-Almeida, X.-L. Huang, S. Hyun, T. Jiang, AAP …

Recoverable gas from hydrate‐bearing sediments: Pore network model simulation and macroscale analyses

J Jang, JC Santamarina - Journal of geophysical research …, 2011 - Wiley Online Library
The volume of hydrate expands into a significantly larger volume of water and gas upon
dissociation. Gas recovery and capillary‐trapped residual gas saturation are investigated by …

[HTML][HTML] Expedition 385 summary

A Teske, D Lizarralde, TW Höfig… - Proceedings of the …, 2021 - publications.iodp.org
International Ocean Discovery Program (IODP) Expedition 385 drilled organic-rich
sediments and intruded sills in the off-axis region and axial graben of the northern spreading …

Strike-slip motion of a mega-splay fault system in the Nankai oblique subduction zone

T Tsuji, J Ashi, Y Ikeda - Earth, Planets and Space, 2014 - Springer
We evaluated the influence of the trench-parallel component of plate motion on the active
fault system within the Nankai accretionary wedge from reflection seismic profiles, high …