An overview of recent (1988 to 2014) caldera unrest: Knowledge and perspectives

V Acocella, R Di Lorenzo, C Newhall… - Reviews of …, 2015 - Wiley Online Library
Calderas are among the most active and dangerous volcanoes. Caldera unrest is defined by
enhanced seismicity, gravity changes, surface deformation, and degassing. Although much …

Triggering of volcanic eruptions by large earthquakes

T Nishimura - Geophysical Research Letters, 2017 - Wiley Online Library
When a large earthquake occurs near an active volcano, there is often concern that volcanic
eruptions may be triggered by the earthquake. In this study, recently accumulated, reliable …

Spatial distribution of intrinsic and scattering seismic attenuation in active volcanic islands–I: model and the case of Tenerife Island

J Prudencio, E Del Pezzo… - Geophysical Journal …, 2013 - academic.oup.com
The complex volcanic system of Tenerife Island is known to have a highly heterogeneous
character, as recently confirmed by velocity tomography. We present new information …

A physical model of sill expansion to explain the dynamics of unrest at calderas with application to Campi Flegrei

F Giudicepietro, G Macedonio, M Martini - Frontiers in Earth Science, 2017 - frontiersin.org
Many calderas show remarkable unrest, which often does not culminate in eruptions (non-
eruptive unrest). In this context the interpretation of the geophysical data collected by the …

Depth and evolution of a silicic magma chamber: Melting experiments on a low-K rhyolite from Usu volcano, Japan

A Tomiya, E Takahashi, N Furukawa… - Journal of …, 2010 - academic.oup.com
We estimated the depth of the magma chamber system beneath Usu volcano, one of the
most active volcanoes in Japan, by melting experiments on the eruptive product of the ad …

Spatial distribution of intrinsic and scattering seismic attenuation in active volcanic islands–II: Deception Island images

J Prudencio, JM Ibáñez… - Geophysical Journal …, 2013 - academic.oup.com
In this work, we present regional maps of the inverse intrinsic quality factor (Q i− 1), the
inverse scattering quality factor (Q s− 1) and total inverse quality factor (Q t− 1) for the …

Shallow resistivity structure of Asama Volcano and its implications for magma ascent process in the 2004 eruption

K Aizawa, Y Ogawa, T Hashimoto, T Koyama… - Journal of Volcanology …, 2008 - Elsevier
Asama volcano is an active volcano with many historical records of Vulcanian eruptions. Its
most recent eruptions occurred in 2004 at the summit crater. In this paper, we argue the …

Shallow velocity structure beneath the Aira caldera and Sakurajima volcano as inferred from refraction analysis of the seismic experiment in 2008 (< Special Section> …

H MIYAMACHI, C TOMARI, H YAKIWARA… - Bulletin of the …, 2013 - jstage.jst.go.jp
We performed refraction analysis for the first P-wave arrival time data observed in the
seismic experiment in 2008, and estimated a shallow velocity model up to 3 km depth …

Seismic tomography at Popocatépetl volcano, Mexico

P Berger, JL Got, CV González, V Monteiller - Journal of Volcanology and …, 2011 - Elsevier
We performed the first 3D seismic tomography of the Popocatépetl volcano, Mexico, from the
inversion of the P-wave arrival times of nearly 1500 earthquakes recorded by up to 11 …

TOMO-ETNA experiment at Etna volcano: activities on land

JM Ibáñez, A Díaz-Moreno, J Prudencio… - Annals of …, 2016 - gfzpublic.gfz-potsdam.de
In the present paper we describe the on-land field operations integrated in the TOMO-ETNA
experiment carried out in June-November 2014 at Mt. Etna volcano and surrounding areas …