ABSTRACT The classical theory of porous media is based on assumed micro‐homogeneity of the solid phase (skeleton). Based on the drained macroscale elastic stiffness, it is possible to analytically compute auxiliary properties such as the Biot‐Willis and Skempton parameters.
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Risk-sensitive mean-field control of large-scale UAV Swarms for stochastic disaster tracking and robust first response. [PDF]
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Thrust-dominated unilateral rupture of a blind listric fault associated with the 2024 Hualien earthquake. [PDF]
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Investigating the universal character of k-M slope in earthquake catalogs from the Visibility Graph method. [PDF]
Scudero S, D'Alessandro A.
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Statistical Characteristics of Strong Earthquake Sequence in Northeastern Tibetan Plateau. [PDF]
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Coseismic crustal seismic velocity changes associated with the 2024 Mw 7.5 Noto earthquake, Japan
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The Earthquake Swarms of Nagusa and Vicinity
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Earthquake swarms occur at many locations all over the world. In most cases, they do not occur just once but happen rather repeatedly at a particular location. We compared intraplate earthquake swarm regions, especially the Vogtland/Western Bohemia area, with plate margins, leading to the conclusion of a fluid triggered earthquake swarm mechanism which
Jochen H Kurz +2 more
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