Eugeniusz Majewski (36 results)

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  • Language: English

    Published by Springer, 2010

    3642087957 / 9783642087950

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  • Language: English

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  • Language: English

    Published by Berlin, Springer, 2008

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    Hardcover. Condition: Gut. 293 S. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. w10636 9783540683544 Sprache: Englisch Gewicht in Gramm: 550.

  • Language: English

    Published by San Diego, Academic Press, 2001

    0126851859 / 9780126851854

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    Hardcover. Condition: Gut. 674 S. Ehem. Bibliotheksexemplar mit Signatur und Stempel. GUTER Zustand, ein paar Gebrauchsspuren. Ex-library with stamp and library-signature. GOOD condition, some traces of use. w10774 9780126851854 Sprache: Englisch Gewicht in Gramm: 1100.

  • Language: English

    Published by Springer Verlag, 2006

    3540313362 / 9783540313366

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    rilegato. Condition: Perfetto (Mint). Book.

  • Language: English

    Published by Springer, 2008

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  • Language: English

    Published by Springer, 2008

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  • Language: English

    Published by Springer, 2008

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  • Language: English

    Published by Springer, 2010

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  • Language: English

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    Language: English

    Published by Springer, 2010

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    Taschenbuch. Condition: Neu. Physics of Asymmetric Continuum: Extreme and Fracture Processes | Earthquake Rotation and Soliton Waves | Roman Teisseyre (u. a.) | Taschenbuch | xvi | Englisch | 2010 | Springer | EAN 9783642087950 | Verantwortliche Person für die EU: Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg, juergen[dot]hartmann[at]springer[dot]com | Anbieter: preigu. …

  • Language: English

    Published by Springer Berlin Heidelberg, 2008

    3642087957 / 9783642087950

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    Paperback. Condition: Brand New. 310 pages. 9.25x6.10x0.71 inches. In Stock.

  • Language: English

    Published by Springer, 2006

    3540313362 / 9783540313366

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  • Language: English

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    Taschenbuch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - Our new monograph has been inspired by the former one, Earthquake Source Asymmetry, Structural Media, and Rotation Effects (R. Teisseyre, M. Takeo, and E. Majewski, eds, Springer 2006). Some problems, c- cerned primarily but not exclusively with the basic theoretical nature, have appeared to us as worthy of further analysis. Thus, in the present mo- graph we intend to develop new theoretical approaches to the theory of continua that go far beyond the traditional seismological applications. We also try to present the links between the experimental data, the observed rotational seismic waves, and their theoretical evaluation and description. In addition, we consider the basic point motions and deformations, and we intend to find the invariant forms to describe such point motions. We believe that there must exist the basic equations for all point motions and deformations, and we derive such relations within a frame of a continuum theory. Thus, in the considered standard asymmetric theory, we include relations not only for the displacement velocities but also for a spin motion and basic point deformations as well. We include here the axial point - formation and twist point deformation represented by the string-string and string-membrane motions. A twist vector is defined here as a vector p- pendicular to the string-string plane and representing its magnitude. It - comes an important counterpart to spin and a key to the presented theory. We show in the forthcoming chapters that the twist motion describes the oscillations of shear axes.…

  • Language: English

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    3642087957 / 9783642087950

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  • Language: English

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  • Language: English

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  • Language: English

    Published by Springer, 2010

    364206843X / 9783642068430

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  • Language: English

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    Taschenbuch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - When thinking, at the beginning of the new century, on our horizons in seismology, we might return to the old question related to the seismic ro- tion effects and waves. Seismology, with its spectacular achievements instrumentation, data processing, seismic tomography and source process theories - remains practically confined to linear ideal elasticity (isotropic or anisotropic). Numerous renown seismologists have tried to go beyond this horizon. As concerns rotation waves, such attempts were inspired by numerous macroscopic observations pointing out the rotation effects, often observed on the ground surface. However, this problem has been app- ently closed by Mallet in 1862, who gave the following explanation: ro- tions of a body on the surface are due to a sequence of impacts of different seismic phases emerging under different angles. Later on, in 1937, I- mura underlined an influence of different inertia moments of an inflicted body. Thus, the surface rotation effects - rotation of some objects on the ground surface - were explained as being caused by the consecutive inc- nations and recovery of these objects to the vertical, when hit by the in- dent seismic body or surface waves. The final position of the object could become slightly twisted in comparison to its former place; the differences between the inertia tensor moments of the object and/or its attachment (as related to friction resistance of binding) to the ground surface play an - portant role.…

  • Language: English

    Published by Springer, Berlin, Springer, 2006

    3540313362 / 9783540313366

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    Buch. Condition: Neu. Druck auf Anfrage Neuware - Printed after ordering - When thinking, at the beginning of the new century, on our horizons in seismology, we might return to the old question related to the seismic ro- tion effects and waves. Seismology, with its spectacular achievements instrumentation, data processing, seismic tomography and source process theories - remains practically confined to linear ideal elasticity (isotropic or anisotropic). Numerous renown seismologists have tried to go beyond this horizon. As concerns rotation waves, such attempts were inspired by numerous macroscopic observations pointing out the rotation effects, often observed on the ground surface. However, this problem has been app- ently closed by Mallet in 1862, who gave the following explanation: ro- tions of a body on the surface are due to a sequence of impacts of different seismic phases emerging under different angles. Later on, in 1937, I- mura underlined an influence of different inertia moments of an inflicted body. Thus, the surface rotation effects - rotation of some objects on the ground surface - were explained as being caused by the consecutive inc- nations and recovery of these objects to the vertical, when hit by the in- dent seismic body or surface waves. The final position of the object could become slightly twisted in comparison to its former place; the differences between the inertia tensor moments of the object and/or its attachment (as related to friction resistance of binding) to the ground surface play an - portant role.…

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  • Language: English

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    Hardcover. Condition: gut. 2006. Earthquake Source Asymmetry, Structural Media and Rotation Effects In deutscher Sprache. pages.

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    Published by Springer Berlin Heidelberg Okt 2010, 2010

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    Taschenbuch. Condition: Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -Our new monograph has been inspired by the former one, Earthquake Source Asymmetry, Structural Media, and Rotation Effects (R. Teisseyre, M. Takeo, and E. Majewski, eds, Springer 2006). Some problems, c- cerned primarily but not exclusively with the basic theoretical nature, have appeared to us as worthy of further analysis. Thus, in the present mo- graph we intend to develop new theoretical approaches to the theory of continua that go far beyond the traditional seismological applications. We also try to present the links between the experimental data, the observed rotational seismic waves, and their theoretical evaluation and description. In addition, we consider the basic point motions and deformations, and we intend to find the invariant forms to describe such point motions. We believe that there must exist the basic equations for all point motions and deformations, and we derive such relations within a frame of a continuum theory. Thus, in the considered standard asymmetric theory, we include relations not only for the displacement velocities but also for a spin motion and basic point deformations as well. We include here the axial point - formation and twist point deformation represented by the string-string and string-membrane motions. A twist vector is defined here as a vector p- pendicular to the string-string plane and representing its magnitude. It - comes an important counterpart to spin and a key to the presented theory. We show in the forthcoming chapters that the twist motion describes the oscillations of shear axes. 312 pp. Englisch. …

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    Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Presents a system approach which combines the physics of asymmetric and degenerated continua with general relativityPresents a system approach which combines the physics of asymmetric and degenerated continua with general relativityIncludes su.…

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    Condition: New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Presents a system approach which combines the physics of asymmetric and degenerated continua with general relativityPresents a system approach which combines the physics of asymmetric and degenerated continua with general relativityIncludes su.…

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    Published by Springer Berlin Heidelberg, Springer Berlin Heidelberg Okt 2010, 2010

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    Taschenbuch. Condition: Neu. This item is printed on demand - Print on Demand Titel. Neuware -Our new monograph has been inspired by the former one, Earthquake Source Asymmetry, Structural Media, and Rotation Effects (R. Teisseyre, M. Takeo, and E. Majewski, eds, Springer 2006). Some problems, c- cerned primarily but not exclusively with the basic theoretical nature, have appeared to us as worthy of further analysis. Thus, in the present mo- graph we intend to develop new theoretical approaches to the theory of continua that go far beyond the traditional seismological applications. We also try to present the links between the experimental data, the observed rotational seismic waves, and their theoretical evaluation and description. In addition, we consider the basic point motions and deformations, and we intend to find the invariant forms to describe such point motions. We believe that there must exist the basic equations for all point motions and deformations, and we derive such relations within a frame of a continuum theory. Thus, in the considered standard asymmetric theory, we include relations not only for the displacement velocities but also for a spin motion and basic point deformations as well. We include here the axial point - formation and twist point deformation represented by the string-string and string-membrane motions. A twist vector is defined here as a vector p- pendicular to the string-string plane and representing its magnitude. It - comes an important counterpart to spin and a key to the presented theory. We show in the forthcoming chapters that the twist motion describes the oscillations of shear axes.Springer Verlag GmbH, Tiergartenstr. 17, 69121 Heidelberg 312 pp. Englisch. …