Dynamics of explosive paroxysms at open-vent andesitic systems: High-resolution mass distribution analyses of the 2006 Tungurahua fall deposit (Ecuador). Earth and Planetary Science Letters, 361, 343-355.

https://doi.org/10.1016/j.epsl.2012.11.002

Causes and consequences of bimodal grain-size distribution of tephra fall deposited during the August 2006 Tungurahua eruption (Ecuador). Bulletin of Volcanology, 74(1), 187-205.

https://doi.org/10.1007/s00445-011-0517-5

Sedimentology and geomorphology of the deposits from the August 2006 pyroclastic density currents at Tungurahua volcano, Ecuador. Bulletin of Volcanology, 75(11), 1-21.

https://doi.org/10.1007/s00445-013-0765-7

Dune bedforms produced by dilute pyroclastic density currents from the August 2006 eruption of Tungurahua volcano, Ecuador. Bulletin of Volcanology, 75(11), 1-20.

https://doi.org/10.1007/s00445-013-0762-x

Large-scale inflation of Tungurahua volcano (Ecuador) revealed by Persistent Scatterers SAR interferometry. Geophysical Research Letters, 41(16), 5821-5828.

https://doi.org/10.1002/2014GL060956

Los depósitos de ceniza del 04-05 de mayo 2013 en el volcán Tungurahua. Pyroclastic Flow, Journal of Geology, 3(1), 1-7.

Stratovolcano growth by co-eruptive intrusion: The 2008 eruption of Tungurahua Ecuador: INSAR OF 2008 ERUPTION OF TUNGURAHUA. Geophysical Research Letters, 37(21),

https://doi.org/10.1029/2010GL044942

Mass budget partitioning during explosive eruptions: insights from the 2006 paroxysm of Tungurahua volcano, Ecuador. Geochemistry, Geophysics, Geosystems.

https://doi.org/10.1002/2016GC006431

Pyroclastic flow erosion and bulking processes: comparing field-based vs. modeling results at Tungurahua volcano, Ecuador. Bulletin of volcanology, 76(9), 858.

Influence of the wind direction variability on the quantification of tephra fallouts: December 2012 and March 2013 Tungurahua eruptions. Avances en Ciencias e Ingenierías, 5(1), A14-A21.

Homemade ashmeter: a low-cost, high-efficiency solution to improve tephra field-data collection for contemporary explosive eruptions. Journal of Applied Volcanology, 2(1), 1.

https://doi.org/10.1186/2191-5040-2-1

The milling factory: Componentry-dependent fragmentation and fines production in pyroclastic flows. Geology, 44(11), 907-910.

Quantifying entrainment in pyroclastic density currents from the Tungurahua eruption, Ecuador: Integrating field proxies with numerical simulations. Geophysical Research Letters, 43(13), 6932-6941.

Adapting to changes in volcanic behaviour: Formal and informal interactions for enhanced risk management at Tungurahua Volcano, Ecuador. Global Environmental Change, 45, 217-226.

Degassing patterns of Tungurahua volcano (Ecuador) during the 1999–2006 eruptive period, inferred from remote spectroscopic measurements of SO2 emissions. Journal of Volcanology and Geothermal Research, 176(1), 151-162.

https://doi.org/10.1016/j.jvolgeores.2008.07.007

Estimating rates of decompression from textures of erupted ash particles produced by 1999-2006 eruptions of Tungurahua volcano, Ecuador. Geology, 40(7), 619-622.

https://doi.org/10.1130/G32948.1

Risk reduction through community-based monitoring: the vigías of Tungurahua, Ecuador. Journal of Applied Volcanology, 3(1), 11.

https://doi.org/10.1186/s13617-014-0011-9

Petrological analysis of the pre-eruptive magmatic process prior to the 2006 explosive eruptions at Tungurahua volcano (Ecuador). Journal of Volcanology and Geothermal Research, 199(1-2), 69-84.

https://doi.org/10.1016/j.jvolgeores.2010.10.010

Source constraints of Tungurahua volcano explosion events. Bulletin of Volcanology, 68(5), 480-490.

https://doi.org/10.1007/s00445-005-0023-8

Eruption Source Parameters for forecasting ash dispersion and deposition from vulcanian eruptions at Tungurahua volcano: Insights from field data from the July 2013 eruption. Journal of Volcanology and Geothermal Research, 309, 1-13.

https://doi.org/10.1016/j.jvolgeores.2015.11.001