Advancing Energy Materials by In Situ Atomic Scale Methods
Progress in in situ atomic scale methods leads to an improved understanding of new and advanced energy materials, where a local understanding of complex, inhomogeneous systems or interfaces down to the atomic scale and quantum level is required. Topics from photovoltaics, dissipation losses, phase transitions, and chemical energy conversion are ...
Christian Jooss +21 more
wiley +1 more source
Development of Fault Similar Material for Model Test of Fault Water Inrush Disaster. [PDF]
Li Z +6 more
europepmc +1 more source
From foreshock to mainshock: transient sliding velocity sets nucleation time
Fryer B +3 more
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Study on the range of influence of faults on overburden fissures in the working face under repetitive mining action. [PDF]
Kang X, Ma Y, Hu J, Xu Z, Zeng Y, Li C.
europepmc +1 more source
Multiobjective optimization of CO<sub>2</sub> injection under geomechanical risk in high water cut oil reservoirs using artificial intelligence approaches. [PDF]
Meng F +7 more
europepmc +1 more source
Maximum size and magnitude of injection-induced slow slip events. [PDF]
Sáez A, Passelègue F, Lecampion B.
europepmc +1 more source
A Knowledge-Guide Data-Driven Model with Selective Wavelet Kernel Fusion Neural Network for Gearbox Intelligent Fault Diagnosis. [PDF]
Zhuang N, Ren Z, Yang D, Tian X, Wang Y.
europepmc +1 more source
Quantitative analysis of ultra-close fault dynamic rupture and seismic risks in deep roadway excavation. [PDF]
Li Y, Gao X.
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Related searches:
Fractals, Fault-Gouge, and Friction
pure and applied geophysics, 1989The particle-size distribution of a natural fault-gauge has been determined over the range from 5 μm to 40 cm. The gouge is self-similar over the range from 5 μm to 1 cm having a fractal dimension of 2.60 ± 0.11. The lower and upper fractal limits were also determined.
Charles G. Sammis, Ronald L. Biegel
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Frictional constraints on crustal faulting
Journal of Geophysical Research: Solid Earth, 1996We consider how variations in fault frictional properties affect the phenomenology of earthquake faulting. In particular, we propose that lateral variations in fault friction produce the marked heterogeneity of slip observed in large earthquakes. We model these variations using a rate‐ and state‐dependent friction law, where we differentiate velocity ...
John Boatwright, Massimo Cocco
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