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  • 1
    Call number: IASS 19.92281
    Type of Medium: Monograph available for loan
    Pages: 236 Seiten , 22 cm
    Edition: 1. Auflage
    ISBN: 9783455005288 , 3455005284
    Uniform Title: Identity
    Language: German
    Branch Library: IASS
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  • 2
    Monograph available for loan
    Monograph available for loan
    Tsukuba : National Research Institute for Earth Science and Disaster Prevention
    Associated volumes
    Call number: M 19.95290
    In: Technical note of the National Research Institute for Earth Science and Disaster Prevention
    Type of Medium: Monograph available for loan
    Pages: 1 v. (various pagings) , ill., maps (some col.) , 1 CD-ROM (digital ; 4 3/4 in.) , 30 cm.
    Series Statement: Technical note of the National Research Institute for Earth Science and Disaster Prevention 234
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 3
    Unknown
    Basel, Boston, Berlin : Birkhäuser
    Keywords: earthquake generation process ; earthquake source physics ; earthquake statistics for forecasting ; hazard caused large earthquakes and tsunamis ; numerical simulation studies ; propagation of seismic waves and tsunamis
    Description / Table of Contents: This book presents a series of numerical simulation studies of the earthquake generation process and the evaluation of the hazards caused by large earthquakes and tsunamis, drawn from three distinct topical areas. First, recent research results on earthquake source physics are introduced, which can be used as input for hazard evaluation studies. Then, propagation of seismic waves and tsunamis is discussed, connecting what happens at the source with the resulting damage. Finally, earthquake statistics for forecasting are discussed, a practical application of our knowledge for the mitigation of earthquake and tsunami disasters. This book is suitable for graduate students who are interested in the earthquake generation process and its application in the future. It also will serve researchers who want or need to know how to evaluate the damage due to earthquakes and tsunamis.
    Pages: Online-Ressource (VI, 246 Seiten)
    ISBN: 9783034805872
    Language: English
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  • 4
    Monograph available for loan
    Monograph available for loan
    London : Profile Books
    Call number: PIK D 021-12-0163
    Description / Table of Contents: Contents: Part I: Before the state ; 1. The necessity of politics ; 2. The state of nature ; 3. The tyranny of cousins ; 4. Tribal societies: property, justice, war ; 5. The coming of the leviathan ; Part II: State building ; 6. Chinese tribalism ; 7. War and the rise of the Chinese state ; 8. The great Han System ; 9. Political decay and the return of patrimonial gevernment ; 10. The Indian detour ; 11. Varnas and Jatis ; 12. Weaknesses of Indian polities ; 13. Slavery and the Muslim exit from tribalism ; 14. The Mamluks save Islam ; 15. The functioning and decline of the Ottoman state ; 16. Christianity undermines the family ; Part III: The rule of law ; 17. The origins of the rule of law ; 18. The church becomes a state ; 19. The state becomes a church ; 20. Oriental despotism ; 21. Stationary bandits ; Part IV: Accountable government ; 22. The rise of political accountability ; 23. Rente seekers ; 24. Patrimonialism crosses the Atlantic ; 25. East of the Elbe ; 26. Toward a more perfect absolutism ; 27. Taxation and representation ; 28. Why accountability? Why absolutism ; Part V: Toward a theory of political development ; 29. Political development and political decay ; 30. Political development, then and now
    Type of Medium: Monograph available for loan
    Pages: XIV, 585 S. : graph. Darst., Kt.
    Edition: paperback ed.
    ISBN: 9781846682575
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 5
    Monograph available for loan
    Monograph available for loan
    Dt. Taschenbuch-Verl. : [München]
    Call number: PIK E 700-03-0080
    Type of Medium: Monograph available for loan
    Pages: 460 S.
    ISBN: 3423362715
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 6
  • 7
    Publication Date: 2020-02-12
    Description: We have developed a near-field tsunami forecast system based on an automatic centroid moment tensor (CMT) estimation using regional broadband seismic observation networks in the regions of Indonesia, the Philippines, and Chile. The automatic procedure of the CMT estimation has been implemented to estimate tsunamigenic earthquakes. A tsunami propagation simulation model is used for the forecast and hindcast. A rectangular fault model based on the estimated CMT is employed to represent the initial condition of tsunami height. The forecast system considers uncertainties due to two possible fault planes and two possible scaling laws and thus shows four possible scenarios with these associated uncertainties for each estimated CMT. The system requires approximately 15 min to estimate the CMT after the occurrence of an earthquake and approximately another 15 min to make the tsunami forecast results including the maximum tsunami height and its arrival time at the epicentral region and near-field coasts available. The retrospectively forecasted tsunamis were evaluated by the deep-sea pressure and tide gauge observations, for the past eight tsunamis (M w 7.5–8.6) that occurred throughout the regional seismic networks. The forecasts ranged from half to double the amplitudes of the deep-sea pressure observations and ranged mostly within the same order of magnitude as the maximum heights of the tide gauge observations. It was found that the forecast uncertainties increased for greater earthquakes (e.g., M w 〉 8) because the tsunami source was no longer approximated as a point source for such earthquakes. The forecast results for the coasts nearest to the epicenter should be carefully used because the coasts often experience the highest tsunamis with the shortest arrival time (e.g., 〈30 min).
    Language: English
    Type: info:eu-repo/semantics/article
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  • 8
    Publication Date: 2017-04-04
    Description: On October 31, 2002 a ML=5.4 earthquake occurred in southern Italy, at the margin between the Apenninic thrust belt (to the west) and the Adriatic plate (to the east). In this area, neither historical event nor seismogenic fault is reported in the literature. In spite of its moderate magnitude, the earthquake caused severe damage in cities close to the epicenter and 27 people, out of a total of 29 casualties, were killed by the collapse of a primary school in S. Giuliano di Puglia. By inverting broadband regional waveforms, we computed moment tensor solutions for 15 events, as small as ML=3.5 (Mw=3.7). The obtained focal mechanisms show pure strike-slip geometry, mainly with focal planes oriented to NS (sinistral) and EW (dextral). In several solutions focal planes are rotated counterclockwise, in particular for later events, occurring west of the mainshock. From the relocated aftershock distribution, we found that the mainshock ruptured along an EW plane, and the fault mechanisms of some aftershocks were not consistent with the mainshock fault plane. The observed stress field, resulting from the stress tensor inversion, shows a maximum principal stress axis with an east–west trend (N83°W), whereas the minimum stress direction is almost N–S. Considering both the aftershock distribution and moment tensor solutions, it appears that several pre-existing faults were activated rather than a single planar fault associated with the mainshock. The finite fault analysis shows a very simple slip distribution with a slow rupture velocity of 1.1 km/s, that could explain the occurrence of a second mainshock about 30 h after. Finally, we attempt to interpret how the Molise sequence is related to the normal faulting system to the west (along the Apennines) and the dextral strike-slip Mattinata fault to the east.
    Description: Published
    Description: 141-154
    Description: reserved
    Keywords: waveform modeling ; source parameters ; stress field ; southern Apennines ; 04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneous
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Format: 937391 bytes
    Format: application/pdf
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  • 9
    Publication Date: 2017-04-03
    Description: We propose a new source-time function, to be used in kinematic modeling of ground-motion time histories, which is consistent with dynamic propagation of earthquake ruptures and makes feasible the dynamic interpretation of kinematic slip models. This function is derived from a source-time function first proposed by Yoffe (1951), which yields a traction evolution showing a slip-weakening behavior. In order to remove its singularity, we apply a convolution with a triangular function and obtain a regularized source-time function called the regularized Yoffe function. We propose a parameterization of this slip-velocity time function through the final slip, its duration, and the duration of the positive slip acceleration (Tacc). Using this analytical function, we examined the relation between kinematic parameters, such as peak slip velocity and slip duration, and dynamic parameters, such as slip-weakening distance and breakdown-stress drop. The obtained scaling relations are consistent with those proposed by Ohnaka and Yamashita (1989) from laboratory experiments. This shows that the proposed source-time function suitably represents dynamic rupture propagation with finite slip-weakening distances.
    Description: Published
    Description: 1211–1223
    Description: 3.1. Fisica dei terremoti
    Description: JCR Journal
    Description: partially_open
    Keywords: Earthquake dynamics and mechanics ; Earthquake modeling ; Earthquake parameters ; 04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 10
    Publication Date: 2017-04-04
    Description: In this study we aim to understand the dependence of the critical slip weakening distance (Dc) on the final slip (Dtot) during the propagation of a dynamic rupture and the consistency of their inferred correlation. To achieve this goal we have performed a series of numerical tests suitably designed to validate the adopted numerical procedure and to verify the actual capability in measuring Dc. We have retrieved two kinematic rupture histories from spontaneous dynamic rupture models governed by a slip weakening law in which a constant Dc distribution on the fault plane as well as a constant Dc / Dtot ratio are assumed, respectively. The slip velocity and the shear traction time histories represent the synthetic “real” target data which we aim to reproduce. We use a 3-D traction-at-split nodes numerical procedure to image the dynamic traction evolution by assuming our modeled slip velocity as a boundary condition on the fault plane. We assume a regularized Yoffe function as source time function in our modeling attempts and we measure the critical slip weakening distance from the inferred traction versus slip curves at each point on the fault. We compare the inferred values with those of the target dynamic models. Our numerical tests show that fitting the slip velocity functions of the target models at each point on the fault plane is not enough to retrieve good traction evolution curves and to obtain reliable measures of Dc. We find that the estimation of Dc is very sensitive to any small variation of the slip velocity function. An artificial correlation between Dc/Dtot is obtained when a fixed shape of slip velocity is assumed on the fault (i.e., constant rise time and constant time for positive acceleration) which differs from that of the target model. We point out that the estimation of fracture energy (breakdown work) on the fault is not affected by biases in measuring Dc.
    Description: FIRB-MIUR project Airplane (RBPR05B2ZJ 006)
    Description: Published
    Description: 1205-1220
    Description: 3.1. Fisica dei terremoti
    Description: JCR Journal
    Description: partially_open
    Keywords: Earthquake dynamics ; Earthquake ground motions ; Computational seismology ; Theoretical seismology ; 04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamics
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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