Review of major shale-dominated detachment and thrust characteristics in the diagenetic zone: Part I, meso-and macro-scopic scale

CK Morley, C von Hagke, RL Hansberry… - Earth-Science …, 2017 - Elsevier
There is considerable variability in the thickness, structure, and macroscopic deformation
style within shale-prone major thrust zones, which also impacts the structural style in the …

A review of shallow slow earthquakes along the Nankai Trough

S Takemura, Y Hamada, H Okuda, Y Okada… - Earth, Planets and …, 2023 - Springer
Slow earthquakes occur at deep and shallow plate boundaries along the Nankai Trough.
Deep slow earthquakes are continuously distributed along the 30–40 km depth contours of …

Subducting volcaniclastic-rich upper crust supplies fluids for shallow megathrust and slow slip

AC Gase, NL Bangs, DM Saffer, S Han, PK Miller… - Science …, 2023 - science.org
Recurring slow slip along near-trench megathrust faults occurs at many subduction zones,
but for unknown reasons, this process is not universal. Fluid overpressures are implicated in …

Hydrothermal friction experiments on simulated basaltic fault gouge and implications for megathrust earthquakes

H Okuda, AR Niemeijer, M Takahashi… - Journal of …, 2023 - Wiley Online Library
Nucleation of earthquake slip at the plate boundary fault (décollement) in subduction zones
has been widely linked to the frictional properties of subducting sedimentary facies …

Rapid tremor migration and pore-pressure waves in subduction zones

VM Cruz-Atienza, C Villafuerte, HS Bhat - Nature communications, 2018 - nature.com
Rapid tremor migration (RTM) in subduction zones is a manifestation of complex fault-zone
processes on the plate interface. Recent observations have revealed a large diversity of …

Mapping the geological structures in the Ras El Ush field (Gulf of Suez, Egypt), based on seismic interpretation and 3D modeling techniques

TS Imam, MI Abdel-Fattah, T Tsuji… - Journal of African Earth …, 2022 - Elsevier
Abstract The Ras El Ush field (Gulf of Suez, Egypt) is characterized by various complex
structural features, such as evaporite deposits and faulting. Such complex geologic setting …

Relationship between permeability and resistivity of sheared rock fractures: the role of tortuosity and flow path percolation

K Sawayama, T Ishibashi, F Jiang… - Geophysical Research …, 2023 - Wiley Online Library
The fluid‐flow properties of fractures have received increasing attention regarding the role of
geofluids in the genesis of slow and fast earthquakes and recent advances in …

Structural characteristics of the Nankai Trough shallow plate boundary inferred from shallow very low frequency earthquakes

S Takemura, T Matsuzawa, A Noda… - Geophysical …, 2019 - Wiley Online Library
The spatial distributions of shallow slow earthquakes are related to stress accumulation and
structural characteristics of the shallow plate boundary, which are important for …

[HTML][HTML] Frictional properties of the décollement in the shallow Nankai Trough: constraints from friction experiments simulating in-situ conditions and implications for …

H Okuda, M Kitamura, M Takahashi… - Earth and Planetary …, 2023 - Elsevier
Along subduction zone megathrust faults, the transition from smectite to illite with depth
occurs at temperatures of∼ 150° C and has long been hypothesized to be one of the …

Full waveform inversion of repeating seismic events to estimate time-lapse velocity changes

R Kamei, D Lumley - Geophysical Journal International, 2017 - academic.oup.com
Seismic monitoring provides valuable information regarding the time-varying changes in
subsurface physical properties caused by natural or man-made processes. However, the …