Results 11 to 20 of about 448,903 (200)

The advance in obtaining fault slip rate of strike slip fault-A review

open access: yesEarthquake Research Advances, 2021
Slip rate along the major active fault is an important parameter in the quantitative study of active tectonics. It is the average rate of fault slip during a certain period of time, reflecting the rate of strain energy accumulation on the fault zone.
Jinrui Liu   +4 more
openaire   +2 more sources

Stability of pulse-like earthquake ruptures [PDF]

open access: yes, 2019
Pulse-like ruptures arise spontaneously in many elastodynamic rupture simulations and seem to be the dominant rupture mode along crustal faults. Pulse-like ruptures propagating under steady-state conditions can be efficiently analysed theoretically, but ...
Beeler N. M.   +6 more
core   +3 more sources

Broadband Records of Earthquakes in Deep Gold Mines and a Comparison with Results from SAFOD, California [PDF]

open access: yes, 2009
For one week during September 2007, we deployed a temporary network of field recorders and accelerometers at four sites within two deep, seismically active mines.
Boettcher, Margaret S   +7 more
core   +2 more sources

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

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   +4 more sources

Constraining the long-term evolution of the slip rate for a major extensional fault system in the central Aegean, Greece, using thermochronology [PDF]

open access: yes, 2006
The brittle/ductile transition is a major rheologic boundary in the crust yet little is known about how or if rates of tectonic processes are influenced by this boundary.
Altherr   +57 more
core   +1 more source

Effects of slip, slip rate, and shear heating on the friction of granite [PDF]

open access: yesJournal of Geophysical Research: Solid Earth, 1998
The stability of fault slip is sensitive to the way in which frictional strength responds to changes in slip rate and in particular to the effective velocity dependence of steady state friction Δμss/Δ ln V. This quantity can vary substantially with displacement, temperature and slip rate.
Michael L. Blanpied   +2 more
openaire   +1 more source

Influence of Slip on the Plateau-Rayleigh Instability on a Fibre [PDF]

open access: yes, 2015
The Plateau-Rayleigh instability of a liquid column underlies a variety of fascinating phenomena that can be observed in everyday life. In contrast to the case of a free liquid cylinder, describing the evolution of a liquid layer on a solid fibre ...
Baümchen, Oliver   +8 more
core   +4 more sources

Analysis of Boundary Slip in a Flow with an Oscillating Wall

open access: yes, 2012
Molecular dynamic (MD) simulation is used to study slip at the fluid-solid boundary in an unsteady flow based on the Stokes second problem. An increase in slip is observed in comparison to the steady flow for shear rates below the critical shear rate of ...
Mohseni, Kamran   +1 more
core   +1 more source

Simulations of slip flow on nanobubble-laden surfaces [PDF]

open access: yes, 2010
On microstructured hydrophobic surfaces, geometrical patterns may lead to the appearance of a superhydrophobic state, where gas bubbles at the surface can have a strong impact on the fluid flow along such surfaces.
Benzi R   +18 more
core   +3 more sources

Home - About - Disclaimer - Privacy