The El Asnam 1980 October 10 inland earthquake: a new hypothesis of tsunami generation
暂无分享,去创建一个
Hélène Hébert | Pierre Briole | P. Briole | H. Hébert | J. Ruegg | Jean Roger | J. Roger | Jean-Claude Ruegg
[1] E. Daskalaki,et al. TSUNAMIS GENERATED BY COASTAL AND SUBMARINE LANDSLIDES IN THE MEDITERRANEAN SEA , 2007 .
[2] D. Wells,et al. New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement , 1994, Bulletin of the Seismological Society of America.
[3] P. Heinrich,et al. Far‐field simulation of tsunami propagation in the Pacific Ocean: Impact on the Marquesas Islands (French Polynesia) , 2001 .
[4] Giorgio Bellotti,et al. Transient response of harbours to long waves under resonance conditions , 2007 .
[5] C. Vita-Finzi,et al. Active folding in the Algerian earthquake of 10 October 1980 , 1981, Nature.
[6] Models of the complex source of the El Asnam earthquake , 1982 .
[7] G. King,et al. Active tectonics of the Algerian Atlas Mountains‐evidence from aftershocks of the 1980 El Asnam earthquake , 1989 .
[8] Obdulia Fernández de Ybarra,et al. Implications of long waves in harbor management: The Gijón port case study , 2008 .
[9] B. Bornhold,et al. The landslide tsunami of November 3, 1994, Skagway Harbor, Alaska , 1996 .
[10] Steven N. Ward,et al. Landslide tsunami , 2003 .
[11] H. Hébert,et al. The Transoceanic 1755 Lisbon Tsunami in Martinique , 2011 .
[12] S. Migeon,et al. Landslide tsunami vulnerability in the Ligurian Sea: case study of the 1979 October 16 Nice international airport submarine landslide and of identified geological mass failures , 2010 .
[13] A. Tarantola,et al. Deformations associated with the El Asnam earthquake of 10 October 1980: Geodetic determination of vertical and horizontal movements , 1982 .
[14] Costas E. Synolakis,et al. Green's law and the evolution of solitary waves , 1991 .
[15] G. King,et al. An aftershock study of the El Asnam (Algeria) earthquake of 1980 October 10 , 1983 .
[16] Ian Parsons,et al. Surface deformation due to shear and tensile faults in a half-space , 1986 .
[17] E. Okal. Seismic parameters controlling far-field tsunami amplitudes: A review , 1988 .
[18] Euan G. C. Smith,et al. Evidence for different scaling of earthquake source parameters for large earthquakes depending on faulting mechanism , 2000 .
[19] Hélène Hébert,et al. The tsunami triggered by the 21 May 2003 Boumerdès-Zemmouri (Algeria) earthquake: field investigations on the French Mediterranean coast and tsunami modelling , 2009 .
[20] H. Hébert,et al. The 1856 Tsunami of Djidjelli (Eastern Algeria): Seismotectonics, Modelling and Hazard Implications for the Algerian Coast , 2009 .
[21] Costas E. Synolakis,et al. Source discriminants for near-field tsunamis , 2004 .
[22] P. Sabatier,et al. Numerical Modelling of a Landslide-generated Tsunami: The 1979 Nice Event , 2000 .
[23] M. Bezzeghoud,et al. Postseismic deformation at El Asnam (Algeria) in the seismotectonic context of northwestern Algeria , 1997 .
[24] V. Gaullier,et al. Deposition processes from echo-character mapping along the western Algerian margin (Oran–Tenes), Western Mediterranean , 2009 .
[25] R. Courant,et al. Über die partiellen Differenzengleichungen der mathematischen Physik , 1928 .
[26] H. Philip,et al. Structural analysis and interpretation of the surface deformations of the El Asnam Earthquake of October 10, 1980 , 1983 .
[27] M. Bezzeghoud,et al. Faulting mechanism of the El Asnam (Algeria) 1954 and 1980 earthquakes from modelling of vertical movements , 1995 .
[28] A. Deschamps,et al. The El Asnam, Algeria, earthquake of 10 October 1980: Multiple-source mechanism determined from long-period records , 1982 .
[29] G. King,et al. The evolution of a thrust fault system: processes of rupture initiation, propagation and termination in the 1980 El Asnam (Algeria) earthquake , 1984 .
[30] A. Mauffret,et al. Consequences of the El-Asnam earthquakes: Turbidity currents and slumps on the Algerian margin (Western Mediterranean) , 1985 .
[31] Said Maouche,et al. The tsunami induced by the 2003 Zemmouri earthquake (MW = 6.9, Algeria): modelling and results , 2006 .
[32] J. Dewey. The 1954 and 1980 Algerian earthquakes: Implications for the characteristic-displacement model of fault behavior , 1991 .
[33] A. Rabinovich. Seiches and Harbor Oscillations , 2009 .
[34] G. Yielding. Control of rupture by fault geometry during the 1980 El Asnam (Algeria) earthquake , 1985 .
[35] Thorne Lay,et al. Rigidity variations with depth along interplate megathrust faults in subduction zones , 1999, Nature.
[36] B. Savoye,et al. Processes of late Quaternary turbidity current flow and deposition on the Var deep‐sea fan, north‐west Mediterranean Sea , 1993 .
[37] N. Ambraseys. The El Asnam (Algeria) earthquake of 10 October 1980; conclusions drawn from a field study , 1981, Quarterly Journal of Engineering Geology.
[38] Susan L. Bilek,et al. Effect of depth‐dependent shear modulus on tsunami generation along subduction zones , 2001 .
[39] H. Philip,et al. Seismotectonics of the El Asnam earthquake , 1981, Nature.
[40] E. Okal. Normal Mode Energetics for Far-field Tsunamis Generated by Dislocations and Landslides , 2003 .
[41] Y. Okada. Surface deformation due to shear and tensile faults in a half-space , 1985 .
[42] G. Pedersen,et al. Mechanisms of tsunami generation by submarine landslides - a short review , 2006 .
[43] N. Sultan,et al. Submarine Landslides Along the Algerian Margin: A Review of Their Occurrence and Potential Link with Tectonic Structures , 2010 .
[44] M. Kasser,et al. Deformations associated with the El Asnam earthquake of October 10, 1980 (Algeria) , 1987 .
[45] H. Hébert,et al. The 1755 Lisbon Tsunami in Guadeloupe Archipelago: Source Sensitivity and Investigation of Resonance Effects , 2010 .
[46] H. Kanamori,et al. A moment magnitude scale , 1979 .
[47] G. Bertrand,et al. Plio-Quaternary reactivation of the Neogene margin off NW Algiers, Algeria: The Khayr al Din bank , 2009 .
[48] H. Hébert,et al. The 1856 Djijelli (Algeria) earthquake and tsunami: source parameters and implications for tsunami hazard in the Balearic Islands , 2008 .
[49] Philip,et al. Drainage diversions as evidence of propagating active faults: example of the El Asnam and Thenia faults, Algeria , 1998 .
[50] J. Nábělek. Geometry and mechanism of faulting of the 1980 El Asnam, Algeria, earthquake from inversion of teleseismic body waves and comparison with field observations , 1985 .
[51] Maurice Ewing,et al. Orleansville Earthquake and Turbidity Currents , 1955 .
[52] J. Jackson,et al. Relations between surface deformation, fault geometry, seismicity, and rupture characteristics during the El Asnam (Algeria) earthquake of 10 October 1980 , 1981 .
[53] S. Grilli,et al. The Papua New Guinea tsunami of 17 July 1998: anatomy of a catastrophic event , 2008 .
[54] Philip Watts,et al. The Sissano, Papua New Guinea tsunami of July 1998 — offshore evidence on the source mechanism , 2001 .