Determination of cooling rates of glasses over four orders of magnitude
Volcanic materials can experience up to eleven orders of magnitude of cooling rate (qc)
starting from 10–5 K s− 1. The glassy component of volcanic material is routinely measured …
starting from 10–5 K s− 1. The glassy component of volcanic material is routinely measured …
Thermal histories and emplacement dynamics of rhyolitic obsidian lavas at Valles caldera, New Mexico
SM Kenderes, KS Befus, AN Bryson… - Bulletin of Volcanology, 2022 - Springer
The emplacement behaviors and the associated hazards of silicic lavas remain poorly
understood because detailed real-time observations have only been made during a few …
understood because detailed real-time observations have only been made during a few …
[HTML][HTML] The rheology of rhyolite magma from the IDDP-1 borehole and Hrafntinnuhryggur (Krafla, Iceland) with implications for geothermal drilling
Abstract Changes in rhyolite melt viscosity during magma decompression and degassing
exert a first order control on ascent through the crust and volcanic eruption style. These …
exert a first order control on ascent through the crust and volcanic eruption style. These …