In this review paper a set of chemical (H2O, CO2, S, HCl, HF) and water isotopic (δD, δ18O)
data is compiled for 26 subduction zone volcanoes and 3 volcanoes of other tectonic …

The reliable assessment of volcanic unrest must rest on an understanding of the rocks that
form the edifice. It is their microstructure that dictates their physical properties and …

A key question for volcanic hazard assessment is the extent to which information can be
exchanged between volcanoes. This question is particularly pertinent to hazard forecasting …

We investigate the relationship between sulfur and oxygen fugacity at Erta Ale and Masaya
volcanoes. Oxygen fugacity was assessed utilizing Fe3+/∑ Fe and major element …

La mayor parte de los grandes volcanes de nuestro país se encuentran ubicados en la parte
frontal de la Faja Volcánica Transmexicana y en otras zonas volcánicas aisladas. En este …

The failure mode of lava—dilatant or compactant—depends on the physical attributes of the
lava, primarily the porosity and pore size, and the conditions under which it deforms. The …

This chapter describes the practice in the analysis and interpretation of noble gases in
modern hydrothermal systems, including sample collection and analytical methods …

Abstract The World Organization of Volcano Observatories (WOVO), with major support from
the Earth Observatory of Singapore, is developing a web-accessible database of seismic …

Recent phase equilibrium studies, combined with analytical and petrological data, provide
rigorous constraints on the pre-eruptive PTf H 2 0-fO 2-fS 2-fCO 2 conditions of silicic to …

Volcán de Colima (103° 37′ W, 19° 30′ 45 ″N) has had significant eruptive activity over
the last five centuries, leading to its designation as the most active volcano in Mexico. This …