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  • 1
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    In:  Geophys. J. Int., Amsterdam, Elsevier Scientific Publishing Company, vol. 108, no. 33, pp. 767-777, pp. B12308
    Publication Date: 1992
    Keywords: Hypocentral depth ; CRUST ; Seismology ; Geol. aspects ; Tectonics ; Seismicity ; Wahlstroem ; Wahlstrom ; Kulhanek ; GJI
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  • 2
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    In:  Geophys. J. Int., Amsterdam, Elsevier Scientific Publishing Company, vol. 116, no. 33, pp. 377-392, pp. B12308
    Publication Date: 1994
    Keywords: Seismicity ; Tectonics ; Fault plane solution, focal mechanism ; GJI
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  • 3
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    In:  Geophys. J. Int., Minsk, Polish Geothermal Association, vol. 111, no. 3, pp. 577-588, pp. 2339, (ISSN: 1340-4202)
    Publication Date: 1992
    Keywords: Seismicity ; Kulhanek ; GJI
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  • 4
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    Elsevier
    In:  Amsterdam, Elsevier, vol. 1, no. 22, pp. 65-70, (ISBN 3-7643-0253-4)
    Publication Date: 1990
    Keywords: Seismology ; Textbook of geophysics
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Natural hazards 10 (1994), S. 247-259 
    ISSN: 1573-0840
    Keywords: Egypt ; seismic hazard ; maximum expected magnitude ; annual activity ; b-value
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geography , Geosciences
    Notes: Abstract Earthquake hazard parameters such as maximum expected magnitude,M max, annual activity rate,λ, andb value of the Gutenberg-Richter relation have been evaluated for two regions of Egypt. The applied maximum likelihood method permits the combination of both historical and instrumental data. The catalogue used covers earthquakes with magnitude ≥3 from the time interval 320–1987. The uncertainties in magnitude estimates and threshold of completeness were taken into account. The hazard parameter determination is performed for two study areas. The first area, Gulf of Suez, has higher seismicity level than the second, all other active zones in Egypt.b-values of 1.2 ± 0.1 and 1.0 ± 0.1 are obtained for the two areas, respectively. The number of annually expected earthquakes with magnitude ≥3 is much larger in the Gulf of Suez, 39 ± 2 than in the other areas, 6.1 ± 0.5. The maximum expected magnitude is calculated to be 6.5 ± 0.4 for a time span of 209 years for the Gulf of Suez and 6.1 ± 0.3 for a time span of 1667 years for the remaining active areas in Egypt. Respective periods of 10 and 20 years were reported for earthquakes of magnitude 5.0 for the two subareas.
    Type of Medium: Electronic Resource
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  • 6
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    In:  Natural Hazards
    Publication Date: 2020-02-12
    Description: Earthquake hazard parameters such as maximum expected magnitude, Mmax, annual activity rate, lambda, and b value of the Gutenberg-Richter relation have been evaluated for two regions of Egypt. The applied maximum likelihood method permits the combination of both historical and instrumental data. The catalogue used covers earthquakes with magnitude ≥ 3 from the time interval 320-1987. The first area, Gulf of Suez, has higher seismicity level than the second, all other active zones in Egypt. b-values of 1.2 ± 0.1 and 1.0 ± 0.1 are obtained for the two areas, respectively. The number of annually expected earthquakes with magnitude ≥ 3 is much larger in the Gulf of Suez, 39 ± 2 than in the other areas, 6.1 ± 0.5. The maximum expected magnitude is calculated to be 6.5 ± 0.4 for a time span of 209 years for the Gulf of Suez and 6.1 ± 0.3 for a time span of 1667 years for the remaining active areas in Egypt. Respective periods of 10 and 20 years were reported for earthquakes of magnitude 5.0 for the two subareas. -from Authors
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 7
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    In:  Geophysical Journal International
    Publication Date: 2020-02-12
    Description: On 1986 July 14, one of the largest earthquakes in the Baltic Shield during this century occurred near Skovde in the province of Vastergotland, Sweden, with a magnitude of M "SUB L" (UPP) = 4.5. It was followed by the so far largest number of recorded aftershocks, more than 20, from any Swedish earthquake. The strongest aftershock, with M "SUB L" (UPP) = 3.4, occurred about one hour after the main shock. A few months later, on November 2, an M "SUB L" (UPP) - 3.6 event took place near Mariestad some 30 km northwest of the Skovde series. All these shocks were located in the lower crust with foci at depths between 20 and 35 km indicating active movements in the shield at depths where mainly ductile deformation is usually assumed. The calculated seismic moment and stress drop for the Skovde main shock and for the Mariestad earthquake are given. Faulting of the area is shown to be complex, with styles ranging from strike-slip to normal, suggesting that other factors than the push from the North Atlantic Ridge, e.g. post-glacial rebound, also contribute to the lithospheric stress pattern. -from Authors
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 8
    Publication Date: 2020-02-12
    Description: On June 15, 1985, an earthquake with a local magnitude M "SUB L" (UPP) value of 4.6 occurred in the Kattegat area close to the Swedish-Danish border. Two more events occurred in the same area: on April 1, 1986 (M "SUB L" (UPP) = 4.2), and May 24, 1990 (M "SUB L" (UPP) = 3.3). The derived focal mechanisms have north-south trending P-axes which deviate by 45 degrees from the NW-trending compressive stress field postulated by the ridge-push theory. The mechanisms can, however, be explained by local neotectonism. -from Authors
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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