ALBERT — All Library Books, journals and Electronic Records Telegrafenberg

1

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Comparison of frequency of occurrence of earthquakes with slip rates from long-term seismicity data: the cases of Gulf of Corinth, Sea of Marmara and Dead Sea fault zone (2006)

N. N. Ambraseys

In: Geophysical Journal International, Luxembourg, EGS-Gauthier-Villars, vol. 165, no. 2, pp. 516-526, pp. 2214

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Publikationsdatum: 2006

Schlagwort(e): Seismicity ; Recurrence of earthquakes ; Greece ; Israel ; Jordan ; Turkey ; Fault zone ; NAF ; DSTF ; earthquake, ; historical ; seismicity, ; slip ; rates ; GJI

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2

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The size and duration of the Sumatra-Andaman earthquake from far-field static offsets (2005)

P. Banerjee ; F. F. Pollitz ; R. Bürgmann

In: Science, Warszawa, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 308, no. 5729, pp. 1769-1722, pp. 2121

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Publikationsdatum: 2005

Schlagwort(e): Earthquake ; Tsunami(s) ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Source parameters ; Modelling ; Source time function ; Geodesy ; Banda ; Aceh ; Buergmann ; Burgmann ; FROTH

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3

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Submarine fault scarps in the Sea of Marmara pull-apart (North Anatolian Fault): Implications for seismic hazard in Istanbul (2005)

R. Armijo ; N. Pondard ; B. Meyer ; [weitere]

In: Geochem. Geophys. Geosyst., Amsterdam, Elsevier Scientific Publishing Company, vol. 6, no. 6, pp. 1-29, pp. Q06009

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Publikationsdatum: 2005

Beschreibung: Earthquake scarps associated with recent historical events have been found on the floor of the Sea of Marmara, along the North Anatolian Fault (NAF). The MAuto-Regressive Moving Average-processRASCARPS cruise using an unmanned submersible (ROV) provides direct observations to study the fine-scale morphology and geology of those scarps, their distribution, and geometry. The observations are consistent with the diversity of fault mechanisms and the fault segmentation within the north Marmara extensional step-over, between the strike-slip Ganos and Izmit faults. Smaller strike-slip segments and pull-apart basins alternate within the main step-over, commonly combining strike-slip and extension. Rapid sedimentation rates of 1-3 mm/yr appear to compete with normal faulting components of up to 6 mm/yr at the pull-apart margins. In spite of the fast sedimentation rates the submarine scarps are preserved and accumulate relief. Sets of youthful earthquake scarps extend offshore from the Ganos and Izmit faults on land into the Sea of Marmara. Our observations suggest that they correspond to the submarine ruptures of the 1999 Izmit (Mw 7.4) and the 1912 Ganos (Ms 7.4) earthquakes. While the 1999 rupture ends at the immediate eastern entrance of the extensional Cinarcik Basin, the 1912 rupture appears to have crossed the Ganos restraining bend into the Sea of Marmara floor for 60 km with a right-lateral slip of 5 m, ending in the Central Basin step-over. From the Gulf of Saros to Marmara the total 1912 rupture length is probably about 140 km, not 50 km as previously thought. The direct observations of submarine scarps in Marmara are critical to defining barriers that have arrested past earthquakes as well as defining a possible segmentation of the contemporary state of loading. Incorporating the submarine scarp evidence modifies substantially our understanding of the current state of loading along the NAF next to Istanbul. Coulomb stress modeling shows a zone of maximum loading with at least 4-5 m of slip deficit encompassing the strike-slip segment 70 km long between the Cinarcik and Central Basins. That segment alone would be capable of generating a large-magnitude earthquake (Mw 7.2). Other segments in Marmara appear less loaded. FROTH

Schlagwort(e): Earthquake hazard ; Turkey ; Fault zone ; NAF ; G3 ; G-cubed ; AGU ; Ucarkus ; Lepinay ; Cagatay ; Cakir ; Structural geology ; 7230 ; Seismology: ; Seismicity ; and ; tectonics ; Oezalaybey ; Ozalaybey ; Lefevre ; 7223 ; Earthquake ; interaction, ; forecasting, ; and ; prediction ; morphology ; submersible ; 8110 ; Tectonophysics: ; Continental ; tectonics: ; general ; 1766 ; 1894 ; 1912 ; 1999 ; Earthquake

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Überblick

4

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A procedure for source studies from the spectrums of long-period seismic body waves (1965)

A. Ben-Menahem ; S. W. Smith ; T. L. Teng

In: Bull. Seism. Soc. Am., Beijing, Pergamon, vol. 55, no. 17, pp. 203-235, pp. 2135

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Publikationsdatum: 1965

Schlagwort(e): Source mechanics ; Spectrum ; Body waves ; Waves ; Source ; BSSA

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5

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Contiguous rupture areas of two Nankai Trough earthquakes revealed by high-resolution tsunami waveform inversion (2005)

Toshitaka Baba ; Phil R. Cummins

In: Geophys. Res. Lett., Hannover, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 32, no. 8, pp. 281-292, pp. L08305

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Publikationsdatum: 2005

Schlagwort(e): Earthquake ; Tsunami(s) ; Modelling ; Source parameters ; Inversion ; GRL

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Überblick

6

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Crustal attenuation characteristics in northwestern Turkey in the range from 1 to 10 Hz (2006)

D. Bindi ; S. Parolai ; H. Grosser ; [weitere]

In: Bulletin of the Seismological Society of America, Warszawa, Elsevier, vol. 96, no. 1, pp. 200-214, pp. B04312, (ISBN: 0-12-018847-3)

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Publikationsdatum: 2006

Schlagwort(e): Seismology ; Attenuation ; Earthquake hazard ; Fault zone ; NAF ; Spectrum ; BSSA

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Überblick

7

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Field data and satellite imagery of tsunami effects in Banda Aceh (2005)

Jose C. Borrero

In: Science, Leipzig, Birkhäuser Verlag, vol. 308, no. 5728, pp. 1596, pp. L15S17, (ISBN: 0-12-018847-3)

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Publikationsdatum: 2005

Schlagwort(e): Tsunami(s) ; Earthquake ; Indonesia ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; runup ; height ; 〉25 ; m ; reaching ; 3--4 ; km ; inland

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8

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A thermal pressurization model for the spontaneous dynamic rupture propagation on a three-dimensional fault: 2. Traction evolution and dynamic parameters (2006)

A. Bizzarri ; M. Cocco

In: J. Geophys. Res., Warszawa, Elsevier, vol. 111, no. B5, pp. 656-678, pp. B05304, (ISBN: 0-12-018847-3)

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Publikationsdatum: 2006

Schlagwort(e): Modelling ; rate ; state ; Friction ; Stress drop ; Fracture ; Rock mechanics ; Fluids ; Geothermics ; Three dimensional ; Physical properties of rocks ; Source ; Dynamic ; JGR ; dynamic ; fault ; weakening ; frictional ; heating ; pore ; pressure ; evolution ; thermal ; pressurization ; porosity ; 7209 ; Seismology: ; Earthquake ; dynamics ; (1242) ; 7260 ; Theory ; 7290 ; Computational ; seismology

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Überblick

9

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Creeping along the Ismetpasa section of the North Anatolian fault (Western Turkey): Rate and extent from InSAR (2005)

Z. Cakir ; A. M. Akoglu ; S. Belabbes ; [weitere]

In: Earth planet. Sci. Lett., Potsdam, ZIPE, vol. 238, no. 1-2, pp. 225-234, pp. 2156, (ISBN: 0-12-018847-3)

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Publikationsdatum: 2005

Schlagwort(e): Creep observations and analysis ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geodesy ; SAR ; Fault zone ; NAF ; Strike-slip ; EPSL

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10

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Elastic waves radiated by a small source (1967)

K. M. Case ; J. F. Colwell

In: Geophysics, Luxembourg, Conseil de l'Europe, vol. 32, no. 2, pp. 52-59, pp. B04313, (ISBN: 0-12-018847-3)

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Publikationsdatum: 1967

Schlagwort(e): Source ; Seismology ; Waves

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