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楼主: Coagulant
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Magnetism of Rocks and Volumetric Strain in Uniaxial Failure Tests,e-dependent increases in inelastic volumetric strain. In general as the inelastic creep rate increases, the rate of change in remanent magnetization increases. These results suggest that dilatancy related effects of the intensity of rock magnetization should be observed in magnetic rocks in epicentr
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Player and Game State Classes Part 1,toms to arbitrary discrete subgroups of . with compact quotient. The setting of elementary LCA groups is not only an extension of standard Gabor analysis but admits a unified formulation for continuous-time, discrete-time, periodic, and multidimensional signals including the case of nonseparable lattices and/or nonseparable atoms.
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