Results 81 to 90 of about 969,874 (233)
Permeability-controlled migration of induced seismicity to deeper depths near Venus in North Texas
Migration of seismic events to deeper depths along basement faults over time has been observed in the wastewater injection sites, which can be correlated spatially and temporally to the propagation or retardation of pressure fronts and corresponding ...
Kyung Won Chang, Hongkyu Yoon
doaj +1 more source
Slow slip events (SSEs) on the plate interface are closely related to the occurrence of earthquakes and often trigger earthquake swarms in subduction zones.
T. Nishikawa, S. Ide
semanticscholar +1 more source
Human frataxin deficiency causes Friedreich's ataxia, yet how iron‐binding events are communicated across the protein is unclear. Using transfer entropy analysis of molecular dynamics simulations, we identify buried hydrophobic core leucines (LEU136, LEU140) as the source of directional signaling toward the iron‐binding acidic ridge.
Kevser Kübra Kırboğa +1 more
wiley +1 more source
How frictional ruptures and earthquakes nucleate and evolve
Frictional motion is mediated by rapidly propagating ruptures that detach the ensemble of contacts forming the frictional interface between contacting bodies1-7. These ruptures are similar to shear cracks. When this process takes place in natural faults, these rapid ruptures are essentially earthquakes8,9. Although fracture mechanics describe the rapid
Gvirtzman, Shahar +3 more
openaire +3 more sources
An organizational capability framework for earthquake recovery
Engineering and construction capability affects the cost and pace of post-disaster recovery. An organizational capability framework for effective earthquake recovery was developed after studying longitudinally 15 engineering and construction ...
Chang-Richards, Alice +3 more
core +1 more source
FEM simulations of seismic cycle along a complex normal fault
In the assessment and prediction of seismic hazards, developing numerical methods capable of accurately simulating long-term earthquake cycles in complex fault systems is of critical importance.
Zefei Cui, Shoubiao Zhu, Chong Xu
doaj +1 more source
The depth extent of the crustal seismogenic zone is closely related to the size of earthquakes. The mechanisms that control the depth of the lower transition of the seismogenic zone are important issues in seismology and disaster mitigation.
Koji Masuda +2 more
doaj +1 more source
Transformational Faulting: The Case of Quartz‐Coesite
Abstract Transformational faulting in olivine has been widely invoked as a possible triggering mechanism for deep‐focus earthquakes, yet its dynamics remain debated. It is unclear whether it requires the combined effects of heat release, volume change and mechanical strength contrast, or whether it can be triggered by any one of these alone.
Giulia Mingardi +8 more
wiley +1 more source
Understanding the mechanisms of crustal deformation along convergent margins is critical to identifying seismogenic structures and assessing earthquake hazards for nearby urban centers. In the southern central Andes (28–33 $$^{\circ }$$ ∘ S), differences
Jean-Baptiste Ammirati +3 more
doaj +1 more source
Earthquake nucleation on faults with nonconstant normal stress [PDF]
[1] Previous studies have found that earthquake nucleation on faults with rate-and-state dependent constitutive properties is a time dependent process involving evolution of slip rate v and frictional state variable θ. The evolution of θ is governed by an extended aging law, which accounts for the effects of normal stress variations.
Z. Fang +3 more
openaire +1 more source

