Literatura científica selecionada sobre o tema "San Salvador Earthquake, El Salvador, 1986"

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Artigos de revistas sobre o assunto "San Salvador Earthquake, El Salvador, 1986"

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Lara, Mauricio A. "The San Salvador Earthquake of October 10, 1986—History of Construction Practices in San Salvador." Earthquake Spectra 3, no. 3 (1987): 491–96. http://dx.doi.org/10.1193/1.1585443.

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Construction practice in San Salvador, as in the rest of El Salvador, had remained practically unchanged since the time of Spanish colonization up to around 1942. From then on, building practices from many other countries have been introduced, and they have exerted a major influence. The last four decades can be divided into five stages or periods induced by events such as earthquakes in El Salvador and neighboring countries, as well as the incorporation of foreign codes in lieu of a local one and the introduction of new techniques, such as soil mechanics and microseismic investigation. The in
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Harlow, David H., Randall A. White, Michael J. Rymer, and Salvador Alvarez G. "The San Salvador earthquake of 10 October 1986 and its historical context." Bulletin of the Seismological Society of America 83, no. 4 (1993): 1143–54. http://dx.doi.org/10.1785/bssa0830041143.

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Abstract The San Salvador earthquake of 10 October 1986 resulted in 1500 deaths, 10,000 injuries, and 100,000 people left homeless. The earthquake has a surface-wave magnitude (MS) of 5.4, and using strong-motion data, we estimate a moment magnitude (M6−) of 5.7. Focal mechanisms and aftershock distributions from locally recorded seismic data indicate that the earthquake was caused by near-surface, left-lateral slip on a N25°E-trending fault located directly beneath the city of San Salvador. Although strong ground motion lasted for only 3 to 5 sec, horizontal ground accelerations of up to 0.72
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Morgan, James R., and Sam W. Swan. "The San Salvador Earthquake of October 10, 1986—Performance of Lifelines." Earthquake Spectra 3, no. 3 (1987): 585–607. http://dx.doi.org/10.1193/1.1585447.

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Although the October 10, 1986 San Salvador earthquake was only a moderate event of magnitude 5.4 and the recorded ground motions had a relatively short duration, the high recorded peak accelerations caused substantial damage to lifelines. There was significant and widespread damage to buried lifelines. Long-distance telecommunications facilities were reportedly undamaged, but there was substantial loss of local phone service caused by damage to buildings, failures of equipment racks, and loss of emergency power (tilting of batteries). Power generating facilities (hydroelectric and geothermal)
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Rymer, Michael J. "The San Salvador Earthquake of October 10, 1986—Geologic Aspects." Earthquake Spectra 3, no. 3 (1987): 435–63. http://dx.doi.org/10.1193/1.1585440.

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The San Salvador earthquake struck an area of upper Cenozoic volcanic rocks, consisting of basaltic to silicic flows and tuffs. Tuff deposits constitute the upper 30 m of section below San Salvador; thinner sections are in the hills surrounding the city. Tuffs were important in landslide development during the earthquake and may have amplified ground motion. Faults mapped in the area strike east-west, northwest-southeast, and less distinctly, northeast-southwest and north-south. Ringlike structures formed by volcanic subsidence are also present in the area. No evidence was seen of surface faul
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5

Shakal, Anthony F., Moh-jiann Huang, and Roberto Linares. "The San Salvador Earthquake of October 10, 1986—Processed Strong Motion Data." Earthquake Spectra 3, no. 3 (1987): 465–81. http://dx.doi.org/10.1193/1.1585441.

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Strong-motion records were recovered from nine accelerographs at seven stations of the El Salvador Geotechnical Investigation Center Strong Motion Network following the damaging 5.4 Ms San Salvador earthquake of October 10, 1986. The sites were all within 6 km of the epicenter; peak horizontal accelerations at ground level ranged from 0.32 to 0.72 g. The duration of strong shaking was about 3 seconds at most sites. One 10-story concrete building was instrumented with recorders at the basement, second floor, and roof level. The maximum accelerations recorded at this building were 0.47 g at the
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Bommer, Julian, and Stephen Ledbetter. "The San Salvador earthquake of 10th October 1986." Disasters 11, no. 2 (1987): 83–95. http://dx.doi.org/10.1111/j.1467-7717.1987.tb00620.x.

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Durkin, Michael E., and John Hopkins. "The San Salvador Earthquake of October 10, 1986—Architecture and Urban Planning." Earthquake Spectra 3, no. 3 (1987): 609–20. http://dx.doi.org/10.1193/1.1585448.

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Major damage from the October 10 earthquake was concentrated in and around the capital city of San Salvador. Losses exceeded $900 million, or 25% of El Salvador's 1986 gross domestic product. Poor soil conditions, ineffective land use controls, and inadequate building practices combined with the severe shaking intensity to produce widespread damage to both engineered and nonengineered structures. Residential, institutional, and commercial buildings sustained heavy damage. Nonstructural damage and damage to building contents contributed to economic and operational loss. Government officials are
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8

White, Randall A., David H. Harlow, and Salvador Alvarez. "The San Salvador Earthquake of October 10, 1986—Seismological Aspects and Other Recent Local Seismicity." Earthquake Spectra 3, no. 3 (1987): 419–34. http://dx.doi.org/10.1193/1.1585439.

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The San Salvador earthquake of October 10, 1986 originated along the Central American volcanic chain within the upper crust of the Caribbean Plate. Results from a local seismograph network show a tectonic style main shock-aftershock sequence, with a magnitude, Mw, 5.6. The hypocenter was located 7.3 km below the south edge of San Salvador. The main shock ruptured along a nearly vertical plane toward the north-northeast. A main shock fault-plane solution shows a nearly vertical fault plane striking N32\sz\E, with left-lateral sense of motion. This earthquake is the second Central American volca
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9

Anderson, Raymond W. "The San Salvador Earthquake of October 10, 1986—Review of Building Damage." Earthquake Spectra 3, no. 3 (1987): 497–541. http://dx.doi.org/10.1193/1.1585444.

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Damage to low-rise engineered buildings in San Salvador in the three to six-story height range was major and wide-spread. This can probably be attributed to the small natural periods of vibration associated with low-rise buildings and their response when interacting with the short-period and short-duration earthquake ground motion. Damage to high-rise buildings that have much longer periods of vibration was relatively minor. This paper reviews buildings that appeared to have performed well and describes the heavy damage that occurred to low-rise buildings that performed poorly, including examp
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10

Sauter, Franz F. "The San Salvador Earthquake of October 10, 1986—Structural Aspects of Damage." Earthquake Spectra 3, no. 3 (1987): 563–84. http://dx.doi.org/10.1193/1.1585446.

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The October 10, 1986 San Salvador earthquake caused extensive damage to one- and two-story bahareque-type dwellings and buildings, and the collapse of multistory engineered structures. The study of the effects of the San Salvador earthquake on buildings points out that poor quality materials and workmanship, as well as deficiencies in constructive details, are the cause of severe damage. However, it confirms once again that conceptual errors in design, including the selection of the lateral load resistant system, are the main cause of structural failure of buildings and engineered structures.
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Teses / dissertações sobre o assunto "San Salvador Earthquake, El Salvador, 1986"

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Gariel, Jean-Christophe. "Simulation numérique des mouvements forts en champ proche." Grenoble 1, 1988. http://www.theses.fr/1988GRE10080.

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Dans cette etude, on applique la methode des nombres discrets qui permet le calcul du rayonnement de sources etendues de mecanisme quelconque dans un milieu stratifie. On simule ensuite trois evenements de magnitude moderee, a imperial valley, a san salvador et a kalamata
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Livros sobre o assunto "San Salvador Earthquake, El Salvador, 1986"

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Fuentes, Ricardo. Octubre 10, 1986: !terremoto! s.n.], 2010.

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2

EEFIT. The San Salvador earthquake of 10 October 1986: A field report. EEFIT, 1987.

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3

Lungo, Mario. El terremoto de octubre de 1986 en San Salvador y la situación habitacional de los sectores populares. Confederación Universitaria Centroamericana, Secretaría General, 1987.

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4

Salvador, El. Scientific cooperation, earthquake research: Memorandum of understanding between the United States of America and El Salvador, signed at Reston and San Salvador, April 16 and 24, 1984. Dept. of State, 1991.

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5

Brady, Chuck. San Salvador builds back: The story of the Earthquake Reconstruction Program. U.S. Agency of International Development, 1993.

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6

El Salvador. Ministerio de Planificación y Coordinación del Desarrollo Económico y Social., ed. El Salvador: Terremoto del 10 de octubre de 1986 : evaluación de daños : política y programas de emergencia y reconstrucción. Gobierno de la República de El Salvador, Ministerio de Planificación y Coordinación del Desarrollo Económico y Social, 1986.

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7

Matthews, J., S. D. Cooksey, and R. Alley. Avenues of Sedimentation of Carbonate Skeletal Sands in Rice Bay, San Salvador, Bahamas (Occasional Paper, 1986). Bahamian Field Station, 1986.

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Capítulos de livros sobre o assunto "San Salvador Earthquake, El Salvador, 1986"

1

Clark, Peter. "6. Housing Reconstruction in El Salvador: Low Income Housing and Earthquake Reconstruction in the San Salvador Metropolitan Area." In Developing Building for Safety Programmes. Practical Action Publishing, 1995. http://dx.doi.org/10.3362/9781780444758.006.

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2

Morgan, J. R. "Performance of Buried Lifelines During the 10 October 1986 San Salvador Earthquake." In Structures and Stochastic Methods. Elsevier, 1987. http://dx.doi.org/10.1016/b978-0-444-98955-0.50023-9.

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3

"San Salvador Earthquake, Salvador, 1873." In The Illustrated History of Natural Disasters. Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-3325-3_42.

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