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The experts stressed change was urgent.
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c Coulomb stress change resolved onto NW-striking normal faults.
These stresses change the alignment and the orientation of polymer chains and filler particles.
Reservoir heterogeneity depends on formation lithology, depositional environment and fracture development due to stress changes.
The current data suggest that female vulnerability to stress changes across the lifespan.
The dynamic stress change would be two orders of magnitude higher than the static stress changes.
Calculated Coulomb stress change and normal stress change for each earthquake sequence.
b Temporal changes of the median Coulomb stress change.
d Coulomb stress change resolved onto NW-striking thrust faults.
At (1) a large surface stress change is measured.
The Coulomb stress change is defined as: Δσf = Δτs + μΔσn.
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