Abstract
In this research, we have conducted a numerical simulation to obtain the seismic source, coseismic deformation field, and the tsunami propagation of the great Lima-Peru 1940 earthquake and tsunami, based on macroseismic information and focal mechanism from the literature. The seismic dimensions of our preferred model were set at 162 km×71 km according to VIII isoseismal intensity. The slip distribution is homogeneous with a mean value of 2.7 m. The fault plane orientation was set at strike = 330∘, dip = 20∘, and rake = 90∘. The maximum simulated uplift was 1.27 m and the maximum subsidence was 0.36 m. Due to the proximity of the seismic source to the coast, the city of Huacho was uplifted around 11 cm. The fault plane of the 1940 earthquake was located in the updip near the coast. The maximum tsunami height simulated in Huacho was 1.80 m. We suggest that there is a high tsunamigenic potential near the trench to generate a shallow earthquake.
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References
Barazangi M, Isacks B (1976) Spatial distribution of earthquakes and subduction of the Nazca plate beneath South America. Geol 4:686–692
Beck S, Ruff L (1989) Great earthquakes and subduction along the Peru trench. Phys Earth Planet Inter 57:199–224
Beck S, Nishenko S (1990) Variations in the mode of great earthquake rupture along the Central Peru subduction zone. GRL 17(11):1969–1972
Chlieh M, Perfettini H, Tavera H, Avouac J, Remy D, Nocquet J, Rolandone F, Bondoux F, Gabalda G, Bonvalot S (2011) Interseismic coupling and seismic potential along the Central Andes subduction zone. JGR 116, B12405:21
Dorbath L, Cisternas A, Dorbath C (1990) Assessment of the size of large and great historical earthquakes in Peru. BSSA 80(3):515–576
Imamura F (1996) Review of tsunami simulation with a finite difference method. In: Yeh H, Liu P, Synolakis C (eds) Long-wave Runup Models. World Scientific, Singapore, pp 25–42
Imamura F, Yalciner A, Ozyurt G (2006) Tsunami modelling manual (TUNAMI model). Tohoku University, Japan, p 58. Available on: http://www.tsunami.civil.tohoku.ac.jp/hokusai3/J/projects/manual-ver-3.1.pdf
Ioualalen M, Perfettini H, Yauri S, Jimenez C (2013) Tsunami modeling to validate slip models of the 2007 Mw8.0 Pisco earthquake, Central Peru. PAAG 170:433–451. https://doi.org/10.1007/s00024-012-0608-z
Jimenez C, Moggiano N, Mas E, Adriano B, Koshimura S, Fujii Y, Yanagisawa H (2013) Seismic source of 1746 Callao Earthquake from tsunami numerical modelling. JDR 8(2):266–273
Jimenez C, Moggiano N, Mas E, Adriano B, Fujii Y, Koshimura S (2014) Tsunami waveform inversion of the 2007 Peru (8.1 Mw) earthquake. JDR 9(6):954–969
Jimenez C (2018) Seismic source characteristics of the intraslab 2017 Chiapas-Mexico earthquake (Mw 8.2). Phys Earth Planet Inter 280:69–75
Kanamori H (1977) The energy release in great earthquakes. JGR 82(20):2981–2987
Kelleher J (1972) Rupture zones of large South American earthquakes and some predictions. JGR 77(11):2087–2103
Lockridge P (1985) Tsunamis in Peru-Chile. National geophysical data center, Report SE-39, pp 97
Mas E, Adriano B, Pulido N, Jimenez C, Koshimura S (2014) Simulation of tsunami inundation in central Peru from future megathrust earthquake scenarios. JDR 9(6):961–967
Norabuena E, Leffler L, Mao A, Dixon T, Stein S, Sacks S, Ocola L, Ellis M (1998) Space geodetic observations of Nazca-South America convergence across the central andes. Science 279:358
Okada Y (1992) Internal deformation due to shear and tensile faults in a half space. BSSA 82:1018–1040
Okal E, Borrero J, Synolakis C (2006) Evaluation of tsunami risk from regional earthquakes at Pisco, Peru. BSSA 96(5):1634–1648
Papazachos B, Scordilis E, Panagiotopoulus C, Karakaisis G (2004) Global relations between seismic fault parameters and moment magnitude of earthquakes. Bulletin of Geological Society of Greece XXXVI:1482–1489
Ren Z, Ji X, Hou J, Shan D, Zhao L (2018) Source inversion and numerical simulation of 2017 Mw 8.1 Mexico earthquake and tsunami. Nat Hazards 94(3):1163–1185
Silgado E (1978) Historia de los sismos más notables ocurridos en el Perú (1513-1974). Instituto de Geología y Minería, Lima
Villegas J (2016) Active tectonics of Peru: heterogeneous interseismic coupling along the Nazca megathrust, rigid motion of the Peruvian Sliver and subandean shortening accomodation. JGR, pp 24. https://doi.org/10.1002/2016JB013080
Acknowledgments
We are grateful to Mr. Christopher Hatch by the revision of the linguistic aspects of the manuscript.
Funding
This study was financially supported by a research grant from the Universidad Nacional Mayor de San Marcos and from Concytec (Consejo Nacional de Ciencia y Tecnología) of Peru.
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Jiménez, C., Moggiano, N. Numerical simulation of the 1940 Lima-Peru earthquake and tsunami (Mw 8.0). J Seismol 24, 89–99 (2020). https://doi.org/10.1007/s10950-019-09887-2
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DOI: https://doi.org/10.1007/s10950-019-09887-2