Hydrogeology and mechanics of subduction zone forearcs: Fluid flow and pore pressure
At subduction zones, fluid flow, pore pressure, and tectonic processes are tightly
interconnected. Excess pore pressure is driven by tectonic loading and fluids released by …
interconnected. Excess pore pressure is driven by tectonic loading and fluids released by …
Controls on tectonic accretion versus erosion in subduction zones: Implications for the origin and recycling of the continental crust
P Clift, P Vannucchi - Reviews of Geophysics, 2004 - Wiley Online Library
Documenting the mass flux through convergent plate margins is important to the
understanding of petrogenesis in arc settings and to the origin of the continental crust, since …
understanding of petrogenesis in arc settings and to the origin of the continental crust, since …
Elevated fluid pressure and extreme mechanical weakness of a plate boundary thrust, Nankai Trough subduction zone
Pore fluid pressure is a key parameter governing both the shear strength of faults and the
conditions for seismic and tsunamigenic slip on subduction zone megathrusts. However …
conditions for seismic and tsunamigenic slip on subduction zone megathrusts. However …
Origin and evolution of a splay fault in the Nankai accretionary wedge
Subduction zones are often characterized by wedge-shaped sedimentary complexes—
called accretionary prisms—that form when sediments are scraped off the subducting plate …
called accretionary prisms—that form when sediments are scraped off the subducting plate …
New insights into deformation and fluid flow processes in the Nankai Trough accretionary prism: Results of Ocean Drilling Program Leg 190
The Nankai Trough accretionary prism is considered an “end‐member” prism accreting a
coarse terrigenous sediment section in a setting with structural simplicity, unparalleled …
coarse terrigenous sediment section in a setting with structural simplicity, unparalleled …
[PDF][PDF] Characterisation and engineering properties of methane hydrate soils
Methane hydrate soil is a natural soil deposit that contains methane hydrate in its pores.
Methane hydrate is a metastable solid material and it bonds the soil particles together …
Methane hydrate is a metastable solid material and it bonds the soil particles together …
[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 …
Evolution of the Nankai Trough décollement from the trench into the seismogenic zone: Inferences from three-dimensional seismic reflection imaging
We mapped the amplitude of the Nankai Trough subduction thrust seismic reflection from the
trench into the seismogenic zone with three-dimensional seismic reflection data. The …
trench into the seismogenic zone with three-dimensional seismic reflection data. The …
Interplate patchiness and subduction-erosion mechanisms: Evidence from depth-migrated seismic images at the central Ecuador convergent margin
Prestack depth-migrated seismic lines provide accurate images of the convergent
Ecuadorian margin, where the southern flank of the Carnegie Ridge subducts. The margin is …
Ecuadorian margin, where the southern flank of the Carnegie Ridge subducts. The margin is …
Pore pressure development and progressive dewatering in underthrust sediments at the Costa Rican subduction margin: Comparison with northern Barbados and …
DM Saffer - Journal of Geophysical Research: Solid Earth, 2003 - Wiley Online Library
At subduction zones, pore pressure affects fault strength, deformation style, structural
development, and potentially the updip limit of seismogenic faulting behavior through its …
development, and potentially the updip limit of seismogenic faulting behavior through its …