Results 261 to 270 of about 425,010 (300)
Some of the next articles are maybe not open access.
Earthquake‐Scaling Relationships from Geodetically Derived Slip Distributions
Bulletin of the Seismological Society of America, 2019AbstractEmpirical earthquake scaling relationships describe expected relationships between moment magnitude and various spatial descriptors of the earthquake rupture (along‐strike length, down‐dip width, rupture area, and peak and mean slip). These scaling relationships play important roles in many seismological, geological, and hazards‐assessment ...
Clayton M. J. Brengman +3 more
openaire +1 more source
Wall Slip of Narrow Molecular Weight Distribution Polybutadienes
Journal of Rheology, 1989A series of polybutadienes (78,000⩽MW⩽240,000), each with a narrow molecular weight distribution (MW ...
F. J. Lim, W. R. Schowalter
openaire +1 more source
Distribution of angular misfits in fault-slip data
Journal of Structural Geology, 1996The validity and the accuracy of a stress determination method based on fault-slip data inversion depends on how the misfits are defined and processed in the inversion procedure. To characterize major features of fault-slip data, angular misfits are simulated for both inherited faults and conjugate faults.
Pom-Yong Chop +2 more
openaire +1 more source
INTRINSIC MODE FUNCTIONS OF EARTHQUAKE SLIP DISTRIBUTION
Advances in Adaptive Data Analysis, 2010In this paper, empirical mode decomposition technique is used to analyze the spatial slip distribution of five past earthquakes. It is shown that the finite fault slip models exhibit five empirical modes of oscillation. The last intrinsic mode is positive and characterizes the non-stationary mean of the slip distribution.
openaire +1 more source
Distributed Slip Model for Forward Modeling Strong Earthquakes
Bulletin of the Seismological Society of America, 2016We develop a generic finite‐fault source model for simulation of large earthquakes: the distributed slip model (DSM). Six geometric and seven kinematic parameters are used to describe a smooth pseudo‐Gaussian slip distribution, such that slip decays from peak slip within an elliptical rupture patch to zero at the borders of the patch.
Shahar Shani‐Kadmiel +2 more
openaire +1 more source
Distribution of slip along an earthquake fault
Acta Seismologica Sinica, 2004Slip distribution of the 1979 Imperial Valley, 1989 Loma Prieta, 1992 Landers, 1994 Northridge, and 1995 Kobe earthquake shows a piece-wise Gutenberg-Richter’s law. For small slips, the b-value is near to 1; while for large slips, the b-value is larger than 1.
openaire +1 more source
Slip of polydisperse polymers: Molecular weight distribution above and below the plane of slip
AIP Conference Proceedings, 2015When strong slip occurs during the drag flow of highly entangled polybutadienes (PBD) in a sliding plate rheometer equipped with stainless steel parallel plates, a thin film of polymer debris remains on the substrate after the slip. This debris is assumed to be formed by the disentanglement process that occurs in strong slip at a distance of about one ...
Seyed Mostafa Sabzevari +2 more
openaire +1 more source
Multicycle slip distribution along a laboratory fault
Journal of Geophysical Research: Solid Earth, 1991Slip distribution along a laboratory fault, which consists of eight spring‐connected blocks that are elastically driven to slide on a frictional surface, has been examined for a “long” sequence of slip events to test the applicability of some conceptual models proposed recently in the literature.
openaire +1 more source
Slip band distribution in rapid thermally annealed silicon wafers
Journal of Applied Physics, 2012X-ray diffraction imaging of 200 mm diameter (100) oriented double-side polished silicon wafers has revealed that the slip band distribution, following rapid thermal annealing (RTA), has a lower symmetry than predicted from the material crystallography.
Garagorri J. +4 more
openaire +1 more source
Slip distribution of the 1985 Central Chile earthquake
Tectonophysics, 1988Abstract Geodetic elevation changes record the deformation associated with the M s = 7.8, March 3, 1985, Central Chile earthquake. By summing elemental point sources in a half-space and employing a gradient technique with positivity constraints, we resolve the slip distribution on the dislocation surface.
openaire +1 more source

