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  • 1
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: M 14.0133 ; M 14.0159
    Description / Table of Contents: This book presents an innovative new approach to studying source mechanisms of earthquakes, combining theory and observation in a unified methodology, with a key focus on the mechanics governing fault failures. It explains source mechanisms by building from fundamental concepts such as the equations of elasticity theory to more advanced problems including dislocation theory, kinematic models and fracture dynamics. The theory is presented first in student-friendly form using consistent notation throughout, and with full, detailed mathematical derivations that enable students to follow each step. Later chapters explain the widely-used practical modelling methods for source mechanism determination, linking clearly to the theoretical foundations, and highlighting the processing of digital seismological data. Providing a unique balance between application techniques and theory, this is an ideal guide for graduate students and researchers in seismology, tectonophysics, geodynamics and geomechanics, and a valuable practical resource for professionals working in seismic hazard assessment and seismic engineering.
    Type of Medium: Monograph available for loan
    Pages: x, 302 S. : Ill., graph. Darst.
    ISBN: 9781107040274
    Classification:
    Seismology
    Language: English
    Note: Earthquakes and fault motion. pp. 1-21. doi:10.1017/CBO9781139628792.002 --- Processing and analysis of recorded seismic signals. pp. 22-40. doi:10.1017/CBO9781139628792.003 --- Mathematical representation of the source. pp. 41-62. doi:10.1017/CBO9781139628792.004 --- Point source models. pp. 63-89. doi:10.1017/CBO9781139628792.005 --- The seismic moment tensor. pp. 90-107. doi:10.1017/CBO9781139628792.006 --- Determination of point source mechanisms. pp. 108-134. doi:10.1017/CBO9781139628792.007 --- Kinematics of extended sources. pp. 135-162. doi:10.1017/CBO9781139628792.008 --- Determination of source dimensions. pp. 163-188. doi:10.1017/CBO9781139628792.009 --- Simple dynamic models. pp. 189-204. doi:10.1017/CBO9781139628792.010 --- Dynamics of fracture. Homogeneous models. pp. 205-231. doi:10.1017/CBO9781139628792.011 --- Fracture dynamics. Heterogeneous models. pp. 232-258. doi:10.1017/CBO9781139628792.012 --- Modeling earthquakes using fracture dynamics. pp. 259-283. doi:10.1017/CBO9781139628792.013
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: M 12.0186 ; M 12.0215
    Description / Table of Contents: The first worldwide survey of active earthquake faults, providing an important basis for protecting threatened cities in the developing world.Providing the first worldwide survey of active earthquake faults, this book focuses on those described as 'seismic time bombs' - with the potential to destroy large cities in the developing world such as Port au Prince, Kabul, Tehran and Caracas. Leading international earthquake expert, Robert Yeats, explores both the regional and plate-tectonic context of active faults, providing the background for seismic hazard evaluation in planning large-scale projects such as nuclear power plants or hydroelectric dams. He also highlights work done in more advanced seismogenic countries like Japan, the United States, New Zealand and China, providing an important basis for upgrading building standards and other laws in developing nations. The book also explores the impact of major quakes on social development through history. It will form an accessible reference for analysts and consulting firms, and a convenient overview for academics and students of geoscience, geotechnical engineering and civil engineering, and land-use planning. Table of contens: Introduction; 1. Methods and background; 2. Introduction to North America: the Pacific-North America plate boundary; 3. San Andreas System and basin and range; 4. Caribbean Plate and Middle America subduction zone; 5. South America; 6. Africa, Arabia, and Western Europe; 7. Eastern Mediterranean, the Caucasus, and the Middle East; 8. India, the Himalaya, Mainland China, and Central Asia; 9. Japan and the Western Pacific; 10. Southeast Asia, Australia, New Zealand, and Pacific Islands; References; Index.
    Type of Medium: Monograph available for loan
    Pages: xii, 621 S. : Ill., graph. Darst.
    ISBN: 9780521190855
    Classification:
    Seismology
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Cambridge : Cambridge University Press
    Call number: M 16.89755
    Description / Table of Contents: Provides a deeper understanding of earthquake processes, based on laboratory-derived physical laws and formulae, for researchers, professionals and graduate students
    Type of Medium: Monograph available for loan
    Pages: x, 270 S.
    Edition: Online-Ausg. 2013
    ISBN: 9781107030060
    Classification:
    Seismology
    Parallel Title: Print version: The Physics of Rock Failure and Earthquakes
    Language: English
    Note: Contents; Preface; 1 Introduction; 2 Fundamentals of rock failure physics; 2.1 Mechanical properties and constitutive relations; 2.1.1 Elastic deformation; 2.1.2 Ductile deformation; 2.1.3 Fracture; 2.1.4 Friction; 2.2 Basics of rock fracture mechanics; 2.2.1 Energy release rate and resistance to rupture growth; 2.2.2 Stress concentration and cohesive zone model; 2.2.3 Breakdown zone model for shear failure; 2.2.4 j-integral and energy criterion for shear failure; 2.2.5 Relation between resistance to rupture growth and constitutive relation parameters. , 3 Laboratory-derived constitutive relations for shear failure3.1 Shear failure of intact rock; 3.1.1 Method and apparatus used; 3.1.2 Constitutive relations derived from data on the shear failure of intact rock; 3.1.3 Geometric irregularity of shear-fractured surfaces and characteristic length; 3.2 Frictional slip failure on precut rock interface; 3.2.1 Method and apparatus used; 3.2.2 Geometric irregularity of precut fault surfaces and characteristic length; 3.2.3 Constitutive relations derived from data on frictional stick-slip failure. , 3.2.4 Laboratory-derived relationships between physical quantities observed during dynamic slip rupture propagation3.3 Unifying constitutive formulation and a constitutive scaling law; 3.3.1 Unification of constitutive relations for shear fracture and for frictional slip failure; 3.3.2 A constitutive scaling law; 3.3.3 Critical energy required for shear fracture and for frictional stick-slip failure; 3.3.4 Stabilityinstability of the breakdown process; 3.3.5 Breakdown zone size; 3.4 Dependence of constitutive law parameters on environmental factors; 3.4.1 Introduction. , 3.4.2 Dependence of shear failure strength on environmental factors3.4.3 Dependence of breakdown stress drop on environmental factors; 3.4.4 Dependence of breakdown displacement on environmental factors; 4 Constitutive laws for earthquake ruptures; 4.1 Basic foundations for constitutive formulations; 4.2 Rate-dependent constitutive formulations; 4.3 Slip-dependent constitutive formulations; 4.4 Depth dependence of constitutive law parameters; 5 Earthquake generation processes; 5.1 Shear failure nucleation processes observed in the laboratory; 5.1.1 Introduction; 5.1.2 Experimental method. , 5.1.3 Nucleation phases observed on faults with different surface roughnessesRough fault; Smooth fault; Extremely smooth fault; 5.1.4 Scaling of the nucleation zone size; 5.2 Earthquake rupture nucleation; 5.2.1 Seismogenic background; 5.2.2 Physical modeling and theoretical derivation of the nucleation zone size; 5.2.3 Comparison of theoretical relations with seismological data; 5.2.4 Foreshock activity associated with the nucleation process; 5.3 Dynamic propagation and generation of strong motion seismic waves; 5.3.1 Slip velocity and slip acceleration in the breakdown zone. , 5.3.2 The cutoff frequency fs max of the power spectral density of slip acceleration at the source.
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