REPORTE TÉCNICO – UPSE – 27.08.2010
Chunga K., Dumont J.F., Iturralde D., Ordóñez M. (2004). Evidence of a tsunami deposit about 1250 yr B.P., Gulf of Guayaquil, Ecuador. Mem. The 32nd IGC Florence – scientific sessions: abstract-124, Italy Chunga K., Zamudio Y., Egred J., Marín G., Quiñónez M., Iturralde D. (2005a). The 12 Dic, 1953, Earthquake, Ms 7.3, Ecuador-Peru Border Region: A case study for applying the New INQUA Intensity Scale. Abstract Vol. Dark Nature - Rapid natural Change and Human Responses, Final Meeting of the Dark Nature Project, Como, Italy, p. 57-58. Chunga K., León C., Quiñónez M., Benítez S., Montenegro G. (2005b). Seismic Hazard Assessment for Guayaquil City (Ecuador): Insights from Quaternary Geological Data. Abstract Vol. Dark Nature - Rapid natural Change and Human Responses, Final Meeting of the Dark Nature Project, Como, Italy, p. 55-56. Chunga K.,Michetti A.M., Pazmiño N., Martillo C., Romero A.,Quiñonez M., Gruppo di Geologia Ambientale (2009). Estimación de máximos niveles de sismicidad para el litoral ecuatoriano a través de la integración de datos geológicos, sismológicos y sismotectónicos. Revista Internacional Oro y Petróleo (3) in press Chuy T. (2003). Macroseismic of Cuba: its application in seismic hazard assessment. Minería y Geología Nos. 1-2, 44-50. Dumont, J.F., Santana, E., Vilema, W., Pedoja, K., Ordoñez, M., Cruz, M., Jimenez, N. and Zambrano, I. (2005). Morphological and microtectonic analysis of Quaternary deformation from Puna and Santa Clara Islands, Gulf of Guayaquil, Ecuador (South America), Tectonophysics. 399, 331– 350. Deniaud, Y., Baby, P., Basile, C., Ordon˜ez, M., Montenegro, G., Mascle, G., 1999. Opening and tectonic and sedimentary evolution of the Gulf of Guayaquil: Neogene and Quaternary fore-arc basin of the south Ecuadorian Andes. Comptes Rendus de l’Acade´mie des Sciences–Series II A–Earth and Planetary Sciences 328 (3), 181–187. Egred, J. (2008). Historia sísmica del Ecuador. Aún por publicar. Información proporcionada por el Autor. Instituto Geofísico – Escuela Politécnica Nacional. Eguez, A., Alvarado, A., Yepes, H., Machette, M.N., Costa, C.H., Dart, R.L., and Bradley, L.-A., 2003, Database and map of Quaternary faults and folds of Ecuador and its offshore regions: U.S. Geological Survey Open-File Report 03-289. Espinoza J. (1992). Terremotos tsunamigénicos en el Ecuador. Acta Oceanográfica del Pacífico, 7(1), 21-28. Fukushima Y., Tanaka T. (1990). A New Attenuation Relation for Peak Horizontal Acceleration of Strong Earthquake Ground Motion in Japan, Bull.Seism.Soc. Am., Vol. 80, No. 4, 757-783. Gere, J.M., and Shah, H.C. (1984). Terra non ferma. New York: W. H. Freeman and Co., 203 p. Gutscher, M. A., J. Malavieille, S. E. Lallemand, and J. Y. Collot (1999), Tectonic segmentation of the North Andean margin: Impact of the Carnegie Ridge collision, Earth Planet. Sci. Lett., 168, 255–270, 1999. IAEA Safety Standards Series (2002). Evaluation of Seismic Hazards for Nuclear Power Plants. Safety Guide. No. NS-G-3.3. International Atomic Energy Agency. Kanamori, H., and K. C. McNally (1982), Variable rupture mode of the subduction zone along the Ecuador-Colombia coast, Bull. Seismol. Soc. Am., 72, 1241–1253. Kanamori, H., 1977. The energy release in great earthquakes, J. geophys. Res., 82, 2981–2987
Diagnóstico sísmico y análisis estructural con identificación de fenómenos geológicos en el Barrio “2 de Febrero” de Anconcito, Provincia de Santa Elena.
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