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  • 1
    Monograph available for loan
    Monograph available for loan
    The seismicity of Turkey and adjacent areas : a historical review, 1500-1800 (1995)
    Beyoglu, Istanbul : Eren
    Details Availability
    Call number: M 97.0481
    Type of Medium: Monograph available for loan
    Pages: 240 S.
    ISBN: 9757622389
    Classification:
    Seismology
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    A history of Persian earthquakes (1982)
    Cambridge [u.a.] : Cambridge Univ. Press
    Details Availability
    Call number: M 93.0339 ; 12787
    Type of Medium: Monograph available for loan
    Pages: XVII, 219 S.
    ISBN: 052124112X
    Classification:
    B.2.1.
    Language: English
    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
    The seismicity of Egypt, Arabia and the Red Sea : a historical review (1994)
    Cambridge : Cambridge Univ. Press
    Details Availability
    Call number: M 95.0008
    Type of Medium: Monograph available for loan
    Pages: xix, 181 S.
    ISBN: 0521391202
    Classification:
    Seismology
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 4
    Electronic Resource
    Electronic Resource
    Dashti Biaz, Iran, Earthquake of August 1968 (1968)
    [s.l.] : Nature Publishing Group
    Nature 220 (1968), S. 903-904 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] With the agreement of the Government of Iran, Unesco sent a reconnaissance mission to the earthquake area, and magnetic tape recording seismic equipment was flown to Iran by the Royal Air Force. The chief objectives of the mission were to make a preliminary study of the seismological and ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/220903a0
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  • 5
    Electronic Resource
    Electronic Resource
    Large Earthquake Forces on Gravity Dam (1968)
    [s.l.] : Nature Publishing Group
    Nature 219 (1968), S. 1354-1356 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Before the Koyna earthquake, a strong motion accelero-graph had been installed in a gallery in the body of the dam, very near the right abutment. At this point the structure is 31 m high and the instrument is located about 12m above foundation level. The accelerograph is a three-component ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/2191354a0
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  • 6
    Electronic Resource
    Electronic Resource
    The Gediz (Turkey) Earthquake of March 28, 1970 (1970)
    [s.l.] : Nature Publishing Group
    Nature 227 (1970), S. 592-593 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Preliminary results show that the main shock occurred at about 2102 h (GMT) with a computed epicentre at 39-1 N-29-60 E and a focal depth of about 20 km. This was followed by a large number of strong aftershocks, the largest of which are shown in Fig. 1; their epicentres follow the general ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/227592a0
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  • 7
    Electronic Resource
    Electronic Resource
    Earthquake hazard in the Kenya Rift: the Subukia earthquake 1928 (1991)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 105 (1991), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The Subukia Valley earthquake in East Africa, magnitude 6.9, occurred on 1928 January 6. This is a little known earthquake associated with a 38 km long surface break that showed normal faulting with a small component of left lateral motion. Maximum throw was 240 cm with an average along the rupture of less than 100 cm. The earthquake triggered rockfalls and minor landslides and exhibited long-period effects at large distances. Considering the magnitude of the earthquake, the amount of damage it caused was not as great as it could have been. This is directly attributable to the sparsity of dwellings and the inherent resistance to earthquake shaking of the local type of huts. In the process of studying this earthquake, the seismicity of the (Gregory) Kenya Rift Valley has been re-evaluated. It is shown that relatively large but infrequent earthquakes do occur in the Kenya (Gregory) Rift Valley, a slowly extending region of low apparent seismicity, and that the seismic hazard of this part of East Africa, deduced from data of the last 95 years, is significant.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1991.tb03460.x
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  • 8
    Electronic Resource
    Electronic Resource
    Magnitudes of Central American earthquakes 1898–1930 (1995)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 121 (1995), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: This paper presents the results of the calculation of surface-wave magnitudes of Central American earthquakes between 1898 and 1930. Some 168 events are identified for which magnitudes can be calculated either on early Milne instruments or later damped seismographs. This is about six times as many as listed in regional or global catalogues. The locations of the more important events were revised using a combination of instrumental readings and macroseismic information.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1995.tb05732.x
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  • 9
    Electronic Resource
    Electronic Resource
    Seismicity and associated strain of central Greece between 1890 and 1988 (1990)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 101 (1990), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We examined the seismicity of central Greece between 1890 and 1988, using macroseismic and instrumental data, to ask two questions: (1) does the seismicity of this period reveal all the major tectonic structures that are known to be active?; and (2) what are the likely strains associated with the seismicity over this period? Many known active structures have been effectively aseismic for the last hundred years, and even the inclusion of all known large events earlier than 1890 reveals no activity associated with the NE coast of Evia, Gulf of Argos, or graben NE of Mt Parnassos. It is clear that even 100 years’ data are inadequate for either a reasonable assessment of seismic risk or for a confident estimation of maximum magnitude. However, we are aware of no earthquakes in central Greece during the last 200 yr that were larger than Ms 7.0. It is probable that the maximum magnitude is restricted by the maximum length of fault segments, which appears to be around 15-20 km. The earthquakes of Ms≥ 5.8 during 1890-1988 can account for a N-S displacement of around 45-70 cm (with maximum and minimum estimates a factor of two greater and smaller than this) across part of a 1890-1900 triangulation network in central Greece that was resurveyed in 1988. The contribution of smaller events may increase this displacement by about 50 per cent. This cumulative seismic displacement is similar to that estimated from the geodetic work (about 100 cm), but a detailed comparison of the two sets of observations will be reported elsewhere. A re-evaluation of all the important earthquakes of 1890–1988 in central Greece is presented in the Appendix, which summarizes information of use to both earth scientists and engineers.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1990.tb05577.x
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  • 10
    Electronic Resource
    Electronic Resource
    Large-magnitude Central American earthquakes, 1898–1994 (1996)
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 127 (1996), S. 0 
    Details
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We have collected and re-examined macroseismic information for large Central American earthquakes since the beginning of the period of instrumental recording about one hundred years ago, and combined this with a reassessment of early instrumental information to produce a catalogue of 51 events that, we believe includes ail those with magnitudes (Ms) greater than 7.0. We have reassessed surface-wave magnitudes by consulting station bulletins and we have derived a correction that gives an equivalent Ms for events of intermediate depth. We have also developed a regional relationship between Ms and seismic moment, which enables us to estimate the seismic slip rate across the Middle American Trench. Our best estimates give an average slip rate several times smaller than suggested convergence rates, but with the seismic slip in the central segment of the trench almost an order of magnitude smaller than that in the segments on either side. The low seismic slip rate may indicate aseismic crustal deformation
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-246X.1996.tb04046.x
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