Titlebook: Surface Waves in Geomechanics: Direct and Inverse Modelling for Soils and Rocks; Carlo G. Lai,Krzysztof Wilmański Book 2005 CISM Udine 200

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Bettina Alberscal inpainting solver directly into the network. This allows to generate masks for 4K images in around 0.6 s while exceeding the quality of stochastic methods on practically relevant densities. Compared to popular existing approaches, this is an acceleration of up to four orders of magnitude.

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Gérard A. Mauginwe only employ Fourier samples along certain adaptively chosen lines. For two-dimensional signals, an analogous result can be established for samples in generic directions. The number of samples here scales quadratically to the sparsity level of the unknown signal.

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Renato Lancellottae .-norm of both the Jacobian and its inverse, ensuring that the deformation is a bi-Lipschitz homeomorphism. Theoretical results emphasising the mathematical soundness of the model are provided, among which the existence of minimisers, a .-convergence result and an analysis of a suitable numerical

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0254-1971 gy. Nowadays the growing interest in practical applications of surface waves stem from the following two main factors: surface waves are ideal for developing re978-3-211-27740-9978-3-211-38065-9Series ISSN 0254-1971 Series E-ISSN 2309-3706

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Theory of Nonlinear Surface Waves and Solitons,waves of permanent form. In the second case compensation between nonlinearity and dispersion may favor the existence of surface solitary waves of various types including surface SH envelope solitons guided by a thin film glued on the nonlinear substrate, as also solitary Rayleigh waves, with an emph

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Book 2005ries even though the motivation of discoverers of surface waves such as Lord Rayleigh stems from their appearance in geophysics and seismology. Nowadays the growing interest in practical applications of surface waves stem from the following two main factors: surface waves are ideal for developing re

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Experimental Soil Behaviour: its Testing by Waves and Engineering Applications,