TTE150

Modelamiento de lahares para la determinación de las zonas de inundación …

Iverson, R. M., & Ouyang, C. (2015). Entrainment of bed material by Earth-surface mass flows: Review and reformulation of depth-integrated theory. Reviews of Geophysics , 53(1), 27–58. Iverson, R. M., Schilling, S. P., & Vallance, J. W. (1998). Objective delineation of lahar inundation hazard zones. Geological Society of America Bulletin , 110(8), 972-984. Lohmar, S. (2008). Petrología de las Ignimbritas Licán y Pucón (volcán Villarrica) y Curacautín. Tesis para optar al grado de Doctor en Ciencias de la Tierra: Universidad de Chile, Departamento de Geología. Lowe, D. (1979). Sediment gravity flows Their classification and some problems of application to natural flows and deposits. In L. Doyle & O. Pilkey . Geology of continental slopes: Society of Economic Paleontologists and Mineralogists Special Publication , (Vol. 27, pp. 75–82). Lowe, D. (1982). Sediment gravity flows: II. Depositional models with special reference to the deposits of high-density turbidity currents. Journal of Sedimentary Petrology , 52, 279–297. Luca, I., Hutter, K., Kuo, C. Y., & Tai, Y. C. (2009). Two-layer models for shallow avalanche flows over arbitrary variable topography. International Journal of Advances in Engineering Sciences and Applied Mathematics , 1(2–3), 99–121. Major, J. (1997). Depositional processes in large-scale debris-flow experiments. Journal of Geology , 105, 345–366. Manville, V., Major, J. J., & Fagents, S. A. (2013). Modeling lahar behavior and hazards. (S. A. R. M. C. Lopes, Ed.) Modeling Volcanic Processes: The Physics and Mathematics of Volcanism , 300–330. Martínez, C., Miralles-Wilhelm, F., & García-Martínez, R. (2011). Quasithree dimensional two-phase debris flow model accounting for boulder transport. Italian Journal Engineering Geological Environment , 457–466. Martínez, V. (2019). Nuevos Antecedentes de los Productos Volcánicos de las Ignimbritas Máficas (13.4-12.7 ka) del Volcán Llaima 38°42’, 71°44’W, Región de la Araucanía,

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