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  • 1
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Isostasy-Congresses. ; Electronic books.
    Description / Table of Contents: Proceedings of the NATO Advanced Research Workshop, Erice, Italy, July 27-August 4, 1990.
    Type of Medium: Online Resource
    Pages: 1 online resource (705 pages)
    Edition: 1st ed.
    ISBN: 9789401133746
    Series Statement: Nato Science Series C: Series ; v.334
    DDC: 551.1/3
    Language: English
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  • 2
    Online Resource
    Online Resource
    San Diego :Elsevier Science & Technology,
    Keywords: Earthquakes -- Congresses. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (629 pages)
    Edition: 1st ed.
    ISBN: 9780444596116
    Series Statement: Enrico Fermi International School of Physics Series ; v.Volume 85
    Language: English
    Note: Front Cover -- Earthquakes: Observation, Theory and Interpretation -- Copyright Page -- Table of Contents -- Preface -- Chapter 1. Earthquake Source Theory: a Review -- I. Introduction -- II. Seismic-source representation theory -- III. Dynamic fault models -- IV. Seismic-radiation theory -- REFERENCES -- Chapter 2. Studies of the Seismic Source Using Normal-Mode Theory -- 1. Introduction -- 2. Outline of normal-mode theory -- 3. Some simple kinematic models of the seismic source -- 4. Seismic data -- 5. Determination of parameters of seismic source -- REFERENCES -- Chapter 3. Engineering Seismology -- 1. Introduction -- 2. Measurement of strong ground motion -- 3. Characteristics of strong ground motion -- 4. The engineering design problem -- REFERENCES -- Chapter 4. Theory and Application of Synthetic Seismograms -- 1. Introduction -- 2. Source descriptions and generalized ray theory -- 3. Modeling at teleseismic distances -- 4. Modeling regional body waves -- 5. Discussion -- Appendix: General ray theory -- REFERENCES -- Chapter 5. Strong-Motion Seismology -- 1. Introduction -- 2. Outline of the development of kinematic models -- 3. Stochastic models for high-frequency generation -- 4. Review of source parameters relevant to strong-motion seismology -- 5. ƒmax and the scaling law of earthquake source spectra at high frequencies -- 6. Future problems -- REFERENCES -- Chapter 6. Fault Asperities Inferred from Seismic Body Waves -- 1. Introduction -- 2. Asperity model -- 3. P-wave seismograms of large earthquakes -- 4. Examples -- 5. Conclusions -- REFERENCES -- Chapter 7. Measures of Strong Ground Motion Derived from a Stochastic Source Model -- 1. Introduction -- 2. Derivation of basic equations -- 3. Parameter estimation -- 4. Applications and discussion -- 5. Summary and conclusions -- Appendix -- REFERENCES. , Chapter 8. Inversion of Surface Waves -- 1. Introduction -- 2. Brief review of earlier studies -- 3. Moment tensor formalism and the inversion of surface wave data -- 4. New developments in moment tensor inversion of surface waves -- 5. Nonlinear inversions of amplitude data -- 6. Concluding remarks -- REFERENCES -- Chapter 9. Crust-Mantle Structure Inferred from Surface Waves -- 1. Introduction -- 2. Crustal surface waves -- 3. Mantle surface waves -- Chapter 10. Mechanical Models of Slow Source Processes -- 1. Introduction -- 2. Observations of slow source processes -- 3. Rupture characteristics and emitted radiation -- 4. Slow earthquakes in terms of slip-rate-dependent friction and fault heterogeneities -- 5. Slow earthquakes in terms of fault anelasticity -- 6. Conclusions -- REFERENCES -- Chapter 11. Regional Deviation of Earthquake Source Mechanisms from the « Double-Couple » Model -- 1. Introduction -- 2. The data -- 3. Results -- 4.Conclusions -- REFERENCES -- Chapter 12. Design Principles of Electronic Inertial Seismometers -- 1. Mechanical receivers -- 2. Transducers -- 3. Instrumental noise -- 4. Response and dynamic range -- 5. The force-balance principle -- 6. Practical force-balance seismometers -- 7.Conclusion -- REFERENCES -- Chapter 13. The Joint Inversion of Seismic Wave Forms for Lateral Variations in Earth Structure and Earthquake Source Parameters -- 1. Introduction -- 2. The calculation of approximate seismograms in a slightly aspherical model -- 3. A procedure for wave form inversion for aspherical structure -- 4. Numerical experiments in wave form inversion -- REFERENCES -- Chapter 14. Predicting Great Earthquakes -- 1. Introduction -- 2. Seismic gaps and regions of high seismic potential -- 3. Development of better historical records of great earthquakes -- 4. Repeat times of large earthquakes. , 5. Time-predictable model of occurrence times of great earthquakes -- 6. Major asperities associated with plate boundaries -- 7. Long-range precursory activity along subduction zones -- 8. Long-term changes in rates of moderate-size earthquakes in California -- 9. Great asperities and great earthquakes, South California -- 10. Seismicity and stress in San Gorgonio-Cajon knot -- 11. Movements of left-lateral subsidiary faults within great asperities as precursors to great earthquakes on San Andreas fault -- 12. Seismic precursors of large California earthquakes -- REFERENCES -- Chapter 15. Volcanic Earthquakes: Examples from Mount St. Helens -- 1. Introduction -- 2. Data -- 3. Discussion -- 4. Conclusions -- REFERENCES -- Chapter 16. The Use of Earthquake Source Studies in Continental Tectonic Geology -- 1. Introduction -- 2. Regional studies -- 3. The problem of focal depth -- 4. The relation between surface deformation and seismic faulting at depth -- 5. Conclusions -- REFERENCES -- Chapter 17. Earthquakes in Italy in the Last Century -- 1. Introduction -- 2. General features of seismic activity of Italy -- 3. The largest earthquakes of this century -- 4. Long-term earthquake prediction in Italy: state of the art -- REFERENCES -- Chapter 18. The 1908 Messina Earthquake and Related Seismicity -- 1. Italian seismicity -- 2. The 1908 Messina earthquake -- REEFERENCES -- Chapter 19. Tectonics and Seismicity in the Italian Region -- 1. Introduction -- 2. Tectonic instability -- 3. Conclusions -- REFERENCES -- Chapter 20. Use of Space Techniques for Geodesy -- PART I: Introduction -- PART II: Principles of VLBI -- 1. Instrumentation -- 2. Observables -- 3. Information content -- 4. Signals -- 5. Noise -- 6. Data analysis -- PART III: Geodetic Results -- 1. Observations of extragalactic radio sources -- 2. Observations of satellites. , 3. Comparison of techniques -- PART IV: Prospects and Problems -- 1. VLBI -- 2. Laser ranging -- 3. Comparisons -- REFERENCES -- Chapter 21. The State of Stress in the Lithosphere Caused by Topography and Its Isostatic Compensation -- Introduction -- 1. Stress generated by topography and its compensation -- 2. Checks with the seismicity of the Apennines -- 3. Checks with the pattern recognition -- REFERENCES -- Chapter 22. Seismic-Risk Analysis -- 1. Statistic distribution of earthquakes -- 2. Potential earthquake damage -- REFERENCES -- Chapter 23. Global Seismicity -- 1. Large earthquakes in the world -- 2. Temporal variation -- 3. Destructive earthquakes -- 4. Seismicity and plate motion -- REFERENCES -- PROCEEDINGS OF THE INTERNATIONAL SCHOOL OF PHYSICS.
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  • 3
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Geodynamics-Congresses. ; Electronic books.
    Description / Table of Contents: Proceedings of the NATO Advanced Research Workshop, Erice, Sicily, Italy, September 18-27, 1992.
    Type of Medium: Online Resource
    Pages: 1 online resource (434 pages)
    Edition: 1st ed.
    ISBN: 9789401120166
    Series Statement: Nato Science Series C: Series ; v.402
    Language: English
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  • 4
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 122 (1995), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Theoretical relationships allow the distributed deformation due to seismic activity to be quantified on the basis of the analysis of moment tensors. We apply this method to a data set consisting of seismic events that have occurred in the past 85 yr (1908–1992) along the most important seismogenic zones of the Mediterranean region. We use the Centroid Moment Tensor (CMT) Catalog prepared at Harvard University, covering the last 16 yr, and older data from Jackson & McKenzie (1988). We determine the seismic deformation and compare it to estimates of the overall deformation as obtained from global plate motion and geological studies. We generally find that the geometry of seismic deformation is similar to tectonic predictions. Even though spanning a shorter time interval, the CMT Catalog often gives a better estimate of deformation geometry than the whole data set (85 yr). Seismic deformation generally ranges from less than 10 per cent to more than 90 per cent of the total deformation. Uncertainties arise because data sets may not be representative of the long-term seismic behaviour of each zone. More reliable estimates for comparison with geodynamic processes should result from analysis of a longer time period, for which no instrumental data are available. The similarity of the deformation geometry using CMT data with tectonic expectations suggests, for several zones, the possibility of using historical data to infer longer term deformation rates based on current deformation geometry.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Physics of the Earth and Planetary Interiors 43 (1986), S. 223-235 
    ISSN: 0031-9201
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Physics of the Earth and Planetary Interiors 18 (1979), S. 13-19 
    ISSN: 0031-9201
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Physics of the Earth and Planetary Interiors 75 (1992), S. 131-143 
    ISSN: 0031-9201
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Physics of the Earth and Planetary Interiors 84 (1994), S. 289-298 
    ISSN: 0031-9201
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Amsterdam : Elsevier
    Physics of the Earth and Planetary Interiors 33 (1983), S. 226-242 
    ISSN: 0031-9201
    Source: Elsevier Journal Backfiles on ScienceDirect 1907 - 2002
    Topics: Geosciences , Physics
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 351 (1991), S. 53-55 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Estimates of mantle viscosity have been based on postglacial rebound1 and geoid anomalies2. A stratified mantle with a lower-mantle viscosity of ~1022 Pa s is favoured by geoid anomalies2, whereas from global sea-level changes3 a lower-mantle viscosity has been obtained that is slightly higher than ...
    Type of Medium: Electronic Resource
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