Results 191 to 200 of about 107,777 (298)
A Rate‐and‐State Friction Based Criterion for the Probability of Earthquake Fault Jumps
Abstract Geometrical complexities in natural fault zones, such as steps and gaps, pose a challenge in seismic hazard studies as they can act as obstacles to seismic ruptures. In this study, we propose a criterion, which is based on the rate‐and‐state equation, to estimate the efficiency of an earthquake rupture to jump between two spatially ...
Sylvain Michel +7 more
wiley +1 more source
Seismic Isolation Performance of Seismic Metamaterials Based on Embedded Dual-Resonator Coupled Auxetic Materials. [PDF]
Zhang L +6 more
europepmc +1 more source
Abstract We estimated the scaled energy (eR ${e}_{R}$) for small earthquakes (1.5≤Mjma≤3.0 $1.5\mathit{\le }{M}_{\text{jma}}\mathit{\le }3.0$) in the focal area of the 2016 Mw 7.0 Kumamoto earthquake to examine the underlying physical processes governing the foreshocks‐mainshock‐aftershock sequence.
Masaki Orimo +4 more
wiley +1 more source
Studies of Geosphere Interactions by Means of Laser Interference Complex. [PDF]
Dolgikh G, Budrin S, Dolgikh S.
europepmc +1 more source
Abstract The Southern Rocky Mountain Trench (SRMT) is a conspicuous valley in the eastern Canadian Cordillera. It lies above a sharp change in lithospheric strength and thickness and is occupied by a normal fault thought to have last been active in the Eocene.
T. Finley +5 more
wiley +1 more source
Attenuation of surface-related multiples for single-channel seismic survey in offshore engineering. [PDF]
Shen H +7 more
europepmc +1 more source
Abstract In Guatemala, the Cocos, North American, and Caribbean plates interact to create a region of high seismic risk. Previous analyses of crustal faults in the country have been overly simplified, creating discrepancies between geologic and geodetic slip rate models.
Jeremy Maurer +3 more
wiley +1 more source
An electrochemical hypothesis of earthquakes exploring a theoretical link between radiated seismic energy and Pourbaix potential. [PDF]
Das A, Bag SP.
europepmc +1 more source
Abstract Earth's long period background seismic wavefield is dominated by two distinct processes that couple ocean wave energy to a global microseism wavefield. We assess global microseism intensity in the secondary (4–10 s) and primary (14–20 s) bands, and across eight 2 s‐wide period bands between 4 and 20 s.
Richard C. Aster +4 more
wiley +1 more source
A yield design approach to the stability analysis of A seabed subjected to wave loading and pseudo-static seismic forces. [PDF]
Quiuqui JPC, Maghous S.
europepmc +1 more source

