Results 91 to 100 of about 1,202,006 (199)
The evolution of pore fluid pressure ( Pf$P_{\mathrm{f}}$) in the most seaward portion of a subduction accretionary prism plays an essential role in the cycle of tsunamigenic earthquakes. Based on recent geophysical observations, here we propose a testable conceptual model for this evolution for northern Cascadia offshore of Washington.
Tianhaozhe Sun, Kelin Wang
wiley +1 more source
Abstract Relative plate motion in subduction zones transitions from frictional slip to viscous flow with increasing depth and temperature. The frictional‐viscous transition can control the depth extent of megathrust earthquakes and episodic tremor and slip (ETS).
So Ozawa +2 more
wiley +1 more source
Fluid-Sediment Interactions in the Nankai Subduction Zone (NanTroSEIZE): Pore Fluid and Mineralogical Records [PDF]
The Nankai Trough Seismogenic Zone Experiment (IODP), SW Japan, aimed at unraveling hydrologic processes at subduction megathrusts and in situ rock and fluid properties to understand the fault zone behavior during earthquake nucleation and rupture ...
Henry, P. +6 more
core +1 more source
Friction and mineral assemblage measurements from IODP subduction zone samples
We combine here the results of laboratory friction experiments and quantification of mineral assemblage for scientific drilling samples recovered from three particularly well-studied subduction zones: the Nankai Trough (SW Japan), Japan Trench (NE Japan),
Ikari, Matt J +3 more
core +1 more source
Mud volcanoes, common seafloor features in subduction zone forearcs, provide crucial insights into deep hydrogeological systems associated with plate subduction.
Ryuta Arai +6 more
doaj +1 more source
The time‐variable features of interseismic deformation in subduction zones are poorly understood and commonly ignored. Here, by incorporating century‐long leveling data and contemporary global navigation satellite systems (GNSS) velocities, we ...
Shaoyang Li +2 more
doaj +1 more source
Numerous deep short-term slow slip events (S-SSEs) and long-term slow slip events (L-SSEs) have been detected in the Nankai Trough subduction zone in southwestern Japan based on Global Navigation Satellite System (GNSS) data.
Yuji Kikuchi, Yuta Mitsui, Masayuki Kano
doaj +1 more source
The metamorphic evolution of an ancient accretionary prism in the southern zone of the Damara Belt in Namibia [PDF]
The Southern Zone of the Damara Belt in central Namibia has an apparent stratigraphic thickness that exceeds 100 km and is comprised of highly strained, metamorphosed clastic sedimentary rocks that are intercalated with slices of metamorphosed basalt and
Cross, Clayton Basil
core +1 more source
Understanding variations of slip distance along major thrust systems at convergent margins is an important issue for evaluation of near-trench slip and the potential generation of large tsunamis.
Hideki Mukoyoshi +2 more
doaj +1 more source
Les zones de subduction sont le site d’une intense activité sismique et de grandedéformation tectonique. Le pied du prisme d’accrétion ont été longtemps considéréescomme des zones asismiques où l’énergie des séismes de dissipait.
Pwavodi, Joshua Tanihungoama
core

