Silicic Volcanism: Ascent of Viscous Magmas from Crustal Reservoirs ADS Classic is now
deprecated. It will be completely retired in October 2019. This page will automatically redirect to …

One of our aims in the book is to provide geologists with a sound basis for making their own
well founded interpretations. For that reason we cover not only concepts about processes …

High-temperature crystallization domains (HTCDs) including spherulites and lithophysae
form during cooling of silica-rich lava and welded ignimbrites. Spherulites grow in silicate …

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Silicic magma can erupt quietly, as vapour-poor lava, despite petrological evidence that it
once contained ample dissolved water to drive violent venting of tephra. Non-explosive …

Volume 30 of Reviews in Mineralogy introduces in understanding the behavior of magmatic
volatiles and their influence on a wide variety of geological phenomena; in doing this it also …

Deuterium and water contents of rhyolite obsidian tephra clasts and lava flows sampled in
the western USA decrease within each eruptive sequence, from D-and H2O-rich, explosive …

Experimental results and petrologic observations of the eruptive history of Mount Pelée are
integrated, and a model for the magma storage system is presented. Recent (stage 3) …

The growth of lava domes can be either quiescent or violent, with transitions between styles
of behavior commonly occurring with little warning. Here we propose that the behavior …

It is proposed that lava domes possess a yield strength whose magnitude governs their
shape and explosivity. Theoretical and laboratory modelling of the spread of viscoplastic …