Results 21 to 30 of about 67,714 (263)

Slip rate and tremor genesis in Cascadia [PDF]

open access: yesGeophysical Research Letters, 2014
AbstractAt many plate boundaries, conditions in the transition zone between seismogenic and stable slip produce slow earthquakes. In the Cascadia subduction zone, these events are consistently observed as slow, aseismic slip on the plate interface accompanied by persistent tectonic tremor.
Wech, Aaron G, Bartlow, Noel M
openaire   +2 more sources

Slip-rate-dependent friction as a universal mechanism for slow slip events [PDF]

open access: yesNature Geoscience, 2020
A growing body of observations worldwide has documented fault slip transients that radiate little or no seismic energy. The mechanisms that govern these slow slip events (SSEs) and their wide range of depths, slip rates, durations, stress drops and recurrence intervals remain poorly known.
Kyungjae Im   +3 more
openaire   +3 more sources

Effect of Pressure Rate on Rate and State Frictional Slip

open access: yesGeophysical Research Letters, 2020
This paper analyzes the effects of pore pressure rate for a spring - block system that is a simple model of a laboratory experiment. Pore pressure is increased at a constant rate in a remote reservoir and slip is governed by rate and state friction. The frequency of rapid slip events increases with the increase of a nondimensional pressure rate that is
John W. Rudnicki, Yatai Zhan
openaire   +1 more source

Growth Model and Tectonic Significance of the Guman Fold Along the Western Kunlun Mountain Front (Xinjiang, China) Derived From Terrace Deformation and Seismic Data

open access: yesFrontiers in Earth Science, 2020
The activity of blind thrust faults drives fold deformation of overlying strata, leading the folds to be geometrically related to the underlying blind thrust faults.
Jianhong Xu   +8 more
doaj   +1 more source

Mechanical Analysis of Fault Slip Rate Sites within the San Gorgonio Pass Region, Southern California USA

open access: yesTektonika, 2023
Earthquake hazard assessments rely on observations from the field and geophysical data that provide fault slip rate estimates at specific sites and inform the geometry of active faults; however, uncertainty remains for both slip rate and geometry ...
Jennifer Hatch   +2 more
doaj   +1 more source

Environment recognition through laser-range-finder for small exploration rover

open access: yesNihon Kikai Gakkai ronbunshu, 2016
This paper deals with an environment recognition system which is suitable for small-sized autonomous exploration rovers working on a planet far from Earth.
Kai YUN, Shinji HOKAMOTO
doaj   +1 more source

Interseismic Slip and Coupling along the Haiyuan Fault Zone Constrained by InSAR and GPS Measurements

open access: yesRemote Sensing, 2021
The Haiyuan fault zone is an important tectonic boundary and strong seismic activity belt in northeastern Tibet, but no major earthquake has occurred in the past ∼100 years, since the Haiyuan M8.5 event in 1920.
Xin Qiao   +4 more
doaj   +1 more source

Plastic Slip Patterns through Rate-Independent and Rate-Dependent Plasticity

open access: yesKey Engineering Materials, 2014
Plastic deformation induces various types of dislocation microstructures at different length scales, which eventually results in a heterogeneous deformation field in metallic materials. Development of such structures manifests themselves as macroscopic hardening/softening response and plastic anisotropy during strain path changes, which is often ...
Lancioni, Giovanni, Yalcinkaya, Tuncay
openaire   +2 more sources

Present-Day Deformation of the Gyaring Co Fault Zone, Central Qinghai–Tibet Plateau, Determined Using Synthetic Aperture Radar Interferometry

open access: yesRemote Sensing, 2019
Because of the constant northward movement of the Indian plate and blockage of the Eurasian continent, the Qinghai−Tibet Plateau has been extruded by north−south compressive stresses since its formation.
Yong Zhang   +3 more
doaj   +1 more source

Rate-dependent slip boundary conditions for simple fluids [PDF]

open access: yesPhysical Review E, 2007
The dynamic behavior of the slip length in a fluid flow confined between atomically smooth surfaces is investigated using molecular dynamics simulations. At weak wall-fluid interactions, the slip length increases nonlinearly with the shear rate provided that the liquid/solid interface forms incommensurable structures. A gradual transition to the linear
openaire   +5 more sources

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