Source amplitudes of volcano-seismic signals determined by the amplitude source location method as a quantitative measure of event size. Journal of Volcanology and Geothermal Research, 257, 57-71 .

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Interpretation and utility of infrasonic records from erupting volcanoes. Journal of Volcanology and Geothermal Research, 121(1-2), 15-63.

https://doi.org/10.1016/S0377-0273(02)00409-2

Daily monitoring of Ecuadorian volcanic degassing from space. Journal of Volcanology and Geothermal Research, 176(1), 141-150.

https://doi.org/10.1016/j.jvolgeores.2008.01.029

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

Combining historical and 14C data to assess pyroclastic density current hazards in Baños city near Tungurahua volcano (Ecuador). Quaternary International, 394, 98-114.

https://doi.org/10.1016/j.quaint.2015.06.052

A devastating Plinian eruption at Tungurahua volcano reveals formative occupation at ~1100 cal BC in central Ecuador. Radiocarbon, 55(2-3), 1199-1214.

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Impact of tephra falls on Andean communities: The influences of eruption size and weather conditions during the 1999–2001 activity of Tungurahua volcano, Ecuador. Journal of Volcanology and Geothermal Research, 217-218, 91-103.

https://doi.org/10.1016/j.jvolgeores.2011.06.011

The AD 1300–1700 eruptive periods at Tungurahua volcano, Ecuador, revealed by historical narratives, stratigraphy and radiocarbon dating. Journal of Volcanology and Geothermal Research, 176(1), 70-81.

https://doi.org/10.1016/j.jvolgeores.2008.05.019

An approach to source characterization of tremor signals associated with eruptions and lahars. Earth, Planets and Space, 67(1).

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Ascending seismic source during an explosive eruption at Tungurahua volcano, Ecuador. Geophysical Research Letters, 38(1).

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Enhancing volcano‐monitoring capabilities in Ecuador. Eos, Transactions American Geophysical Union, 88(23), 245-246.

Source mechanism of Vulcanian eruption at Tungurahua Volcano, Ecuador, derived fromseismic moment tensor inversions. Journal of Geophysical Research: Solid Earth, 119(2), 1145-1164.

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Acoustic multipole source model for volcanic explosions and inversion for source parameters. Geophysical Journal International, 191(3), 1192-1204.

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Testing the suitability of frictional behaviour for pyroclastic flow simulation by comparison with a well-constrained eruption at Tungurahua volcano (Ecuador). Bulletin of Volcanology, 71(9), 1057-1075.

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Probabilistic analysis of rain-triggered lahar initiation at Tungurahua volcano. Bulletin of Volcanology, 77(8).

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Poor scaling between elastic energy release and eruption intensity at Tungurahua Volcano, Ecuador. Geophysical Research Letters, 32(15).

https://doi.org/10.1029/2005GL022847

SO2 degassing at Tungurahua volcano (Ecuador) between 2007 and 2013: Transition from continuous to episodic activity. Journal of Volcanology and Geothermal Research, 298, 1-14.

https://doi.org/10.1016/j.jvolgeores.2015.03.022

Sequential plug formation, disintegration by Vulcanian explosions, and the generation of granular Pyroclastic Density Currents at Tungurahua volcano (2013–2014), Ecuador. Journal of Volcanology and Geothermal Research, 306, 90-103.

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Pyroclastic density currents (PDC) of the 16–17 August 2006 eruptions of Tungurahua volcano, Ecuador: Geophysical registry and characteristics. Journal of Volcanology and Geothermal Research, 265, 78-93.

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Tungurahua Volcano, Ecuador: structure, eruptive history and hazards. Journal of Volcanology and Geothermal Research, 91(1), 1-21.

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