Centro de Investigación Científica y de Educación Superior de Ensenada, Baja California
Año
Autores / Publicación
Cañón Tapia, E. (2012). Analytical models of magma chamber stability: An abridged critical review of key concepts. Journal of Volcanology and Geothermal Research, 249, 174-196. doi: 10.1016/j.jvolgeores.2012.10.003. (ID: 15741)
Cañón Tapia, E., & Cañón, C. (2012). Geomagnetismo. COSMOS. La Enciclopedia de las Ciencias y la Tecnología en México (pp. 173-179). Universidad Autónoma Metropolitana U. Iztapalapa. (ID: 15738)
Ferre, E., Michelsen, K., Ernst, G., Boyd, J. D., & Cañón Tapia, E. (2012). Vertical zonation of the Barcroft granodiorite, Withe Mountains, California: Implications for magmatic processes. American Mineralogist, 97(7), 1049-1059. doi: 10.2138/am.2012.4013. (ID: 15739)
Cañón Tapia, E. (2011). AMS in granites and lava flows: Two end members of a continuum?. In E.Petrovsky, E.Herrero-Bervera, T. Harinarayana, D.Ivers (Eds.), The Earth's Magnetic Interior (pp. 263-280). Springer. (ID: 15177)
Zhang, S., Cañón Tapia, E., & Walderhaug, H. J. (2011). Magnetic fabric and its significance in the sills and lava flows from Taimyr fold-belt, Arctic Siberia. Tectonophysics, 505(1-4), 68-85. doi: 10.1016/j.tecto.2011.04.004. (ID: 15176)
Cañón Tapia, E., & Cárdenas, K. (2011). Anisotropy of magnetic susceptibility and magnetic properties of obsidians: volcanic implications. International Journal of Earth Sciences. doi: 10.1007/s00531-011-0687-6. (ID: 15178)
Cañón Tapia, E., & Szakács, A. (2010). What is a Volcano?. Geological Society of America. (ID: 12459)
Szakács, A., & Cañón Tapia, E. (2010). Some challenging new perspectives of volcanology. In Cañón-Tapia E., Szakács A. (Eds.), What is a volcano? Special Paper 470 (pp. 123-140). Boulder, CO: Geological Society of America. (ID: 12963)
Cañón Tapia, E. (2010). Origin of large igneous provinces: The importance of a definition. In Cañón-Tapia E., Szakács A. (Eds.), What is a volcano? Special Paper 470 (pp. 77-101). Boulder, CO: Geological Society of America. (ID: 13222)
Negrete Aranda, R., Cañón Tapia, E., Brandle, J. L., Ortega Rivera, M. A., Lee, J., Spelz Madero, R. M., & Hinojosa Corona, A. (2010). Regional orientation of tectonic stress and the stress expressed by post-subduction high-magnesium volcanism in northern Baja California, Mexico: Tectonics and volcanism of San Borja volcanic field. Journal of Volcanology and Geothermal Research, 192(1-2), 97-115. doi: 10.1016/j.jvolgeores.2010.02.014. (ID: 11307)
Cañón Tapia, E. (2009). Hydrostatic principles of volcanic systems. In T. Thordarson, S. Self, G. Larsen, S. K. Rowland and A. Hoskuldsson (Eds.), Studies in Volcanology: The Legacy of George Walker (pp. 267-289). Geological Society of London. (ID: 11270)
Cañón Tapia, E., & Herrero Bervera, E. (2009). Is the Pringle Fallas excursion a product of geomagnetic field behaviour or an artefact of sedimentation processes? Insights from anisotropy of magnetic susceptibility (AMS) analyses. Geophysical Journal International, 178(2), 702-712. doi: 10.1111/J.1365-246X.2009.04223.X. (ID: 13104)
Martín Hernández, F., Cañón Tapia, E., Mattei, M., & Bijaksana, S. (2008). Magnetic anisotropy different scales, different parameters, different stories?. Tectonophysics. doi: 10.1016/j.tecto.2008.11.015. (ID: 11271)
Cañón Tapia, E., & Herrero Bervera, E. (2008). Sampling strategies and the anisotropy of magnetic susceptibility of dykes. Tectonophysics. doi: 10.1016/j.tecto.2008.11.012. (ID: 11272)
Cañón Tapia, E. (2007). How deep can be a dyke?. Journal of Volcanology and Geothermal Research. doi: 10.1016/j.volgeores.2007.11.021. (ID: 9888)