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  • 1
    Book
    Book
    Cambridge [u.a.] :Cambridge Univ. Press,
    UID:
    almahu_BV040803845
    Format: X, 270 S. : , zahlr. graph. Darst., Kt.
    Edition: 1. publ.
    ISBN: 978-1-107-03006-0
    Note: "Physical modelling of earthquake generation processes is essential to further our understanding of seismic hazard. However, the scale-dependent nature of earthquake rupture processes is further complicated by the heterogeneous nature of the crust. Despite significant advances in the understanding of earthquake generation processes, and the derivation of underlying physical laws, controversy remains regarding what the constitutive law for earthquake ruptures ought to be, and how it should be formulated. It is extremely difficult to obtain field data to define physical properties along a fault during a rupture event, at sufficiently high spatial and temporal resolution to resolve the controversy. Instead, laboratory experiments offer a means of obtaining high-resolution measurements that allow the physical nature of shear rupture processes to be deduced. This important new book is written using consistent notation, providing a deeper understanding of earthquake processes from nucleation to their dynamic propagation. Its key focus is a deductive approach based on laboratory-derived physical laws and formulae, such as a unifying constitutive law, a constitutive scaling law, and a physical model of shear rupture nucleation. Topics covered include: the fundamentals of rock failure physics, earthquake generation processes, physical scale dependence, and large-earthquake generation cycles and their seismic activity"-- Provided by publisher.. - Includes bibliographical references and index
    Language: English
    Subjects: Earth Sciences , Geography
    RVK:
    RVK:
    Keywords: Geophysik ; Tektonik ; Seismik ; Kontinentalverschiebung ; Reibung ; Geophysik ; Scherung ; Bruch ; Mathematisches Modell ; Erdbeben ; Seismologie ; Seismik ; Geophysik ; Seismologie ; Erdbeben ; Gebirgsmechanik
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  • 2
    Online Resource
    Online Resource
    Cambridge : Cambridge University Press
    UID:
    gbv_883413116
    Format: 1 Online-Ressource (x, 270 pages) , digital, PDF file(s)
    ISBN: 9781139342865
    Content: Despite significant advances in the understanding of earthquake generation processes and derivation of underlying physical laws, controversy remains regarding the constitutive law for earthquake ruptures and how it should be formulated. Laboratory experiments are necessary to obtain high-resolution measurements that allow the physical nature of shear rupture processes to be deduced, and to resolve the controversy. This important book provides a deeper understanding of earthquake processes from nucleation to their dynamic propagation. Its key focus is a deductive approach based on laboratory-derived physical laws and formulae, such as a unifying constitutive law, a constitutive scaling law, and a physical model of shear rupture nucleation. Topics covered include: the fundamentals of rock failure physics, earthquake generation processes, physical scale dependence, and large-earthquake generation cycles. Designed for researchers and professionals in earthquake seismology, rock failure physics, geology and earthquake engineering, it is also a valuable reference for graduate students
    Note: Title from publisher's bibliographic system (viewed on 05 Oct 2015)
    Additional Edition: ISBN 9781107030060
    Additional Edition: Erscheint auch als Druck-Ausgabe ISBN 9781107030060
    Language: English
    Subjects: Physics
    RVK:
    Keywords: Seismologie ; Erdbeben ; Gebirgsmechanik
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  • 3
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    UID:
    almahu_9948234207602882
    Format: 1 online resource (x, 270 pages) : , digital, PDF file(s).
    ISBN: 9781139342865 (ebook)
    Content: Despite significant advances in the understanding of earthquake generation processes and derivation of underlying physical laws, controversy remains regarding the constitutive law for earthquake ruptures and how it should be formulated. Laboratory experiments are necessary to obtain high-resolution measurements that allow the physical nature of shear rupture processes to be deduced, and to resolve the controversy. This important book provides a deeper understanding of earthquake processes from nucleation to their dynamic propagation. Its key focus is a deductive approach based on laboratory-derived physical laws and formulae, such as a unifying constitutive law, a constitutive scaling law, and a physical model of shear rupture nucleation. Topics covered include: the fundamentals of rock failure physics, earthquake generation processes, physical scale dependence, and large-earthquake generation cycles. Designed for researchers and professionals in earthquake seismology, rock failure physics, geology and earthquake engineering, it is also a valuable reference for graduate students.
    Note: Title from publisher's bibliographic system (viewed on 05 Oct 2015).
    Additional Edition: Print version: ISBN 9781107030060
    Language: English
    Library Location Call Number Volume/Issue/Year Availability
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  • 4
    Book
    Book
    Cambridge [u.a.] : Cambridge Univ. Press
    UID:
    b3kat_BV041183774
    Format: X, 270 S. , graph. Darst.
    ISBN: 9781107030060
    Note: Includes bibliographical references and index
    Language: English
    Subjects: Physics
    RVK:
    Keywords: Erdbeben ; Seismologie ; Seismik ; Geophysik ; Seismologie ; Erdbeben ; Gebirgsmechanik ; Geophysik ; Tektonik ; Seismik ; Kontinentalverschiebung ; Reibung ; Geophysik ; Scherung ; Bruch ; Mathematisches Modell
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  • 5
    Online Resource
    Online Resource
    Cambridge : Cambridge University Press
    UID:
    b3kat_BV042269042
    Format: 1 Online-Ressource (279 Seiten)
    ISBN: 9781107030060 , 9781139342865
    Note: Title from publisher's bibliographic system (viewed on 24 Nov 2014)
    Additional Edition: Erscheint auch als Druck-Ausgabe, Hardcover ISBN 978-1-10-703006-0
    Language: English
    Subjects: Physics , Geography
    RVK:
    RVK:
    Keywords: Geophysik ; Tektonik ; Seismik ; Kontinentalverschiebung ; Reibung ; Geophysik ; Scherung ; Bruch ; Mathematisches Modell ; Erdbeben ; Seismologie ; Seismik ; Geophysik ; Seismologie ; Erdbeben ; Gebirgsmechanik
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  • 6
    AV-Medium
    AV-Medium
    Cambridge : Cambridge University Press
    UID:
    kobvindex_GFZ746772025
    Format: x, 270 S.
    Edition: Online-Ausg. 2013
    ISBN: 9781107030060
    Content: Provides a deeper understanding of earthquake processes, based on laboratory-derived physical laws and formulae, for researchers, professionals and graduate students
    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.
    Additional Edition: ISBN 9781107345713
    Language: English
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  • 7
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    UID:
    edocfu_9959238831102883
    Format: 1 online resource (x, 270 pages) : , digital, PDF file(s).
    Edition: First edition.
    ISBN: 1-107-35783-7 , 1-107-23742-4 , 1-107-34446-8 , 1-107-34921-4 , 1-107-34821-8 , 1-107-34571-5 , 1-107-34196-5 , 1-139-34286-X
    Content: Despite significant advances in the understanding of earthquake generation processes and derivation of underlying physical laws, controversy remains regarding the constitutive law for earthquake ruptures and how it should be formulated. Laboratory experiments are necessary to obtain high-resolution measurements that allow the physical nature of shear rupture processes to be deduced, and to resolve the controversy. This important book provides a deeper understanding of earthquake processes from nucleation to their dynamic propagation. Its key focus is a deductive approach based on laboratory-derived physical laws and formulae, such as a unifying constitutive law, a constitutive scaling law, and a physical model of shear rupture nucleation. Topics covered include: the fundamentals of rock failure physics, earthquake generation processes, physical scale dependence, and large-earthquake generation cycles. Designed for researchers and professionals in earthquake seismology, rock failure physics, geology and earthquake engineering, it is also a valuable reference for graduate students.
    Note: Title from publisher's bibliographic system (viewed on 05 Oct 2015). , 1. Introduction -- 2. Fundamentals of rock failure physics -- 3. Laboratory-derived constitutive relations for shear failure -- 4. Constitutive laws for earthquake ruptures -- 5. Earthquake generation processes -- 6. Physical scale dependence -- 7. Large earthquake generation cycles and accompanying seismic activity -- References -- Index.
    Additional Edition: ISBN 1-108-44571-3
    Additional Edition: ISBN 1-107-03006-4
    Language: English
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