In situ stress state in the Nankai accretionary wedge estimated from borehole wall failures
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 …
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
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 …
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
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 …
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
Travel times recorded onshore from active-source marine seismic surveys were used to
determine Hikurangi forearc wavespeeds. Ray-path midpoints sample forearc crust above …
determine Hikurangi forearc wavespeeds. Ray-path midpoints sample forearc crust above …
Anelastic strain recovery reveals extension across SW Japan subduction zone
Sediment dominated convergent margins typically record substantial horizontal shortening
often associated with great earthquakes. The convergent margin south of Japan is arguably …
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 …
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 …
Kumano forearc basin, as a landward extension of previous drilling in the southwest Japan …
Expedition 349 summary
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 …
Colwell, KA Dadd, W.-W. Ding, I. Hernández-Almeida, X.-L. Huang, S. Hyun, T. Jiang, AAP …
Expedition 385 summary
1. Abstract International Ocean Discovery Program Expedition 385 drilled organic-rich
sediments and intruded sills in the off-axis region and axial graben of the northern spreading …
sediments and intruded sills in the off-axis region and axial graben of the northern spreading …
Recoverable gas from hydrate‐bearing sediments: Pore network model simulation and macroscale analyses
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 …
dissociation. Gas recovery and capillary‐trapped residual gas saturation are investigated by …
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 …
fault system within the Nankai accretionary wedge from reflection seismic profiles, high …