journal article Oct 01, 2006

The Gibraltar Arc seismogenic zone (part 2): Constraints on a shallow east dipping fault plane source for the 1755 Lisbon earthquake provided by tsunami modeling and seismic intensity

Tectonophysics Vol. 426 No. 1-2 pp. 153-166 · Elsevier BV
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References
39
[1]
Argus "Closure of the Africa–Eurasia–North America plate motion circuit and tectonics of the Gloria fault" J. Geophys. Res. (1989) 10.1029/jb094ib05p05585
[2]
Baptista "The 1755 Lisbon; evaluation of the tsunami parameters" J. Geodyn. (1998) 10.1016/s0264-3707(97)00019-7
[3]
Baptista "Constraints on the source of the 1755 Lisbon tsunami inferred from numerical modelling of historical data on the source of the 1755 Lisbon tsunami" J. Geodyn. (1998) 10.1016/s0264-3707(97)00020-3
[4]
Baptista "New study of the 1755 earthquake source based on multi-channel seismic survey data and tsunami modeling" Nat. Hazards Earth Sci. Syst. (2003) 10.5194/nhess-3-333-2003
[5]
Buforn "Seismicity, source mechanisms and tectonics of the Azores–Gibraltar plate boundary" Tectonophysics (1988) 10.1016/0040-1951(88)90031-5
[6]
Calvert "Geodynamic evolution of the lithosphere and upper mantle beneath the Alboran region of the western Mediterranean: constraints from travel time tomography" J. Geophys. Res. (2000) 10.1029/2000jb900024
[7]
Chester "The 1755 Lisbon earthquake" Prog. Phys. Geogr. (2001) 10.1177/030913330102500304
[8]
Fernandes "The relative motion between Africa and Eurasia as derived from ITRF2000 and GPS data" Geophys. Res. Lett. (2003) 10.1029/2003gl017089
[9]
Fukao "Thrust faulting at a lithospheric plate boundary: the Portugal earthquake of 1969" Earth Planet. Sci. Lett. (1973) 10.1016/0012-821x(73)90058-7
[10]
Gjevik "Modeling tsunamis from earthquake sources near Gorringe Bank southwest of Portugal" J. Geophys. Res. (1997) 10.1029/97jc02179
[11]
Gracia "Mapping active faults offshore Portugal (36°N–38°N): implications for seismic hazard assessment along the southwest Iberian margin" Geology (2003) 10.1130/0091-7613(2003)031<0083:mafopn>2.0.co;2
[12]
Gutscher "Evidence for active subduction beneath Gibraltar" Geology (2002) 10.1130/0091-7613(2002)030<1071:efasbg>2.0.co;2
[13]
Gutscher "What caused the Great Lisbon earthquake?" Science (2004) 10.1126/science.1101351
[14]
Hayward "A seismic reflection and GLORIA study of compressional deformation in the Gorringe Bank region, eastern North Atlantic" Geophys. J. Int. (1999) 10.1046/j.1365-246x.1999.00912.x
[15]
Holdahl "Coseismic slip in the 1964 Prince William Sound earthquake: a new geodetic inversion" Pure Appl. Geophys. (1994) 10.1007/bf00875968
[16]
Jimenez-Munt "The transition from linear to diffuse plate boundary in the Azores–Gibraltar region: results from a thin sheet model" Earth Planet. Sci. Lett. (2001) 10.1016/s0012-821x(01)00442-3
[17]
Johnson "The 1964 Prince William Sound earthquake: joint inversion of tsunami and geodetic data" J. Geophys. Res. (1996) 10.1029/95jb02806
[18]
Johnston "Seismic moment assessment of earthquakes in stable continental regions — III. New Madrid, 1811–1812, Charleston 1886 and Lisbon 1755" Geophys. J. Int. (1996) 10.1111/j.1365-246x.1996.tb05294.x
[19]
Lebreiro "Late Quaternary turbidite emplacement on the horseshoe abyssal plain (Iberian margin)" J. Sediment. Res. (1997)
[20]
Levret "The effects of the November 1, 1755 “Lisbon’’ earthquake in Morocco" Tectonophysics (1991) 10.1016/0040-1951(91)90190-4
[21]
Luque "Tsunami deposits as paleoseismic indicators: examples from the Spanish coast" Acta Geol. Hisp. (2001)
[22]
Mader (1988)
[23]
Martinez-Solares "Isoseismal map of the 1755 Lisbon earthquake obtained from Spanish data" Tectonophysics (1979) 10.1016/0040-1951(79)90075-1
[24]
Mendes Victor "Can hydrodynamic modelling of tsunami contribute to seismic risk assessment?" Phys. Chem. Earth (1999) 10.1016/s1464-1895(99)00009-5
[25]
Mourabit, T., Ben Sari, D., Reilinger, R., McClusky, S., Gomez, F., Barazangi, M., 2002. Preliminary evidence of active deformation in Morocco from repeat GPS observations, Proceedings, Wegener 2002 Conference, June 2002, Athens, Greece (abstract).
[26]
Negredo "Neotectonic modeling of the Ibero–Maghrebian region" J. Geophys. Res. (2002) 10.1029/2001jb000743
[27]
Okada "Surface deformation due to shear and tensile faults in a half-space" Bull. Seismol. Soc. Am. (1985) 10.1785/bssa0750041135
[28]
Park "Splay faults branching along the Nankai subduction zone" Science (2002) 10.1126/science.1074111
[29]
Reilinger, R., McClusky, S., Ben Sari, D., Mourabit, T., Gomez, F., Barazangi, M., 2001. Active deformation in Morocco from repeat GPS observations, EOS Trans. AGU, Fall Meeting 2001 suppl., (abstract).
[30]
Sartori "Eastern segment of the Azores–Gibraltar line (central-eastern Atlantic): an oceanic plate boundary with diffuse compressional deformation" Geology (1994) 10.1130/0091-7613(1994)022<0555:esotag>2.3.co;2
[31]
Satake "Fault slip and seismic moment of the 1700 Cascadia earthquake inferred from Japanese tsunami descriptions" J. Geophys. Res. (2003) 10.1029/2003jb002521
[32]
Smith "Global seafloor topography from satellite altimetry and ship depth soundings" Science (1997) 10.1126/science.277.5334.1956
[33]
Terrinha "Tsunamigenic–seismogenic structures, neotectonics, sedimentary processes and slope instability on the Southwest Portugese Margin" Mar. Geol. (2002) 10.1016/s0025-3227(02)00682-5
[34]
Thiebot, E., Gutscher, M.-A., this volume. The Gibraltar Arc seismogenic zone (part 1): constraints on a shallow east dipping fault plane source for the 1755 Lisbon earthquake provided by seismic data, gravity and thermal modeling. Tectonophysics.
[35]
Thomson "An AMS radiocarbon method to determine the emplacement time of recent deep-sea turbidites" Sediment. Geol. (1994) 10.1016/0037-0738(94)90079-5
[36]
Udias "Body and surface wave study of source parameters of the March 15, 1964 Spanish earthquake" Tectonophysics (1970) 10.1016/0040-1951(70)90034-x
[37]
Vilanova "Lisbon 1755: a case of triggered onshore rupture?" Bull. Seismol. Soc. Am. (2003) 10.1785/0120020245
[38]
Wells "New empirical relationships among magnitude, rupture length, rupture width, rupture area and surface displacement" Bull. Seismol. Soc. Am. (1994) 10.1785/bssa0840040974
[39]
Zitellini "Source of 1755 Lisbon earthquake and tsunami investigated" Eos (Transactions, American Geophysical Union) (2001) 10.1029/eo082i026p00285-01
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Published
Oct 01, 2006
Vol/Issue
426(1-2)
Pages
153-166
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M.-A. Gutscher, M.A. Baptista, J.M. Miranda (2006). The Gibraltar Arc seismogenic zone (part 2): Constraints on a shallow east dipping fault plane source for the 1755 Lisbon earthquake provided by tsunami modeling and seismic intensity. Tectonophysics, 426(1-2), 153-166. https://doi.org/10.1016/j.tecto.2006.02.025
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