Año
Autores / Publicación
Contreras Pérez, J., & Negrete Aranda, R. (2014). A 1.5D model of the steady-state thermal structure of detachment folds. Marine and Petroleum Geology, 54, 96-105. doi: 10.1016/j.marpetgeo.2014.02.019. (ID: 16845)
Sclater, J. G., Hasterok, D., Gouturbe , B., Hillier, J., & Negrete Aranda, R. (2014). Marine Heat Flow. In Jan Harff, Martin Meschede, Sven Petersen, Jörn Thiede (Eds.), Encyclopaedia of Marine Geosciences (pp. 16). Springer. (ID: 21575)
Negrete Aranda, R., Contreras Pérez, J., & Spelz Madero, R. M. (2013). Viscous dissipation, slab melting, and post-subduction volcanism in south-central Baja California, Mexico. Geosphere, 9(6), 1714-1728. doi: 10.1130/GES00901.1. (ID: 15287)
Contreras Pérez, J., Ramírez Zerpa, N. A., & Negrete Aranda, R. (2012). Modelos tectonoestratigráficos de las cuencas de Tiburón y Wagner en el norte del Golfo de California. Revista Mexicana de Ciencias Geológicas, 29(1), 140-157. http://satori.geociencias.unam.mx. (ID: 15308)
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)
Negrete Aranda, R., & Cañón Tapia, E. (2007). Post-subduction volcanism in the Baja California Peninsula, Mexico: The effects of tectonic reconfiguration in volcanic systems. Lithos, 102(1), 392-414. doi: 10.1016/j.lithos.2007.08.013. (ID: 9898)
Morales, J., Goguitchaichvili, A., Cañón Tapia, E., & Negrete Aranda, R. (2003). Further absolute geomagnetic paleointensities from Baja California: evaluation of Pliocene and early/middle Pleistocene data. Comptes Rendus Geoscience, 335(14), 995-1004. (ID: 6275)
Goguitchaichvili, A., Morales, J., Cañón Tapia, E., & Negrete Aranda, R. (2003). Geomagnetic field strength during late miocene: first paleointensity results from Baja California. Journal of Geophysical Research, 108(B2), 1-15. (ID: 3381)