An introduction to the application of X-ray microtomography to the three-dimensional study of igneous rocks
Imaging rocks in three-dimensions through X-ray microtomography enables routine
visualization of structures in samples, which can be spatially resolved down to the sub …
visualization of structures in samples, which can be spatially resolved down to the sub …
Open-vent volcanoes fuelled by depth-integrated magma degassing
Open-vent, persistently degassing volcanoes—such as Stromboli and Etna (Italy), Villarrica
(Chile), Bagana and Manam (Papua New Guinea), Fuego and Pacaya (Guatemala) …
(Chile), Bagana and Manam (Papua New Guinea), Fuego and Pacaya (Guatemala) …
Textural studies of vesicles in volcanic rocks: an integrated methodology
Vesicles in volcanic rocks are frozen records of degassing processes in magmas. For this
reason, their sizes, spatial arrangements, numbers and shapes can be linked to physical …
reason, their sizes, spatial arrangements, numbers and shapes can be linked to physical …
Permeability controls on expansion and size distributions of pyroclasts
AC Rust, KV Cashman - Journal of Geophysical Research …, 2011 - Wiley Online Library
We synthesize field and experimental data to evaluate relationships between the textures
and sizes of pyroclasts and the processes that shape them, with emphasis on the role of …
and sizes of pyroclasts and the processes that shape them, with emphasis on the role of …
Shallow vent architecture during hybrid explosive–effusive activity at Cordón Caulle (Chile, 2011–12): evidence from direct observations and pyroclast textures
In June 2011, an eruption of rhyolite magma began at the Puyehue–Cordón Caulle volcanic
complex, southern Chile. By January 2012, explosive activity had declined from sustained …
complex, southern Chile. By January 2012, explosive activity had declined from sustained …
Direct observation of degassing during decompression of basaltic magma
Transitions in eruptive style during volcanic eruptions strongly depend on how easily gas
and magma decouple during ascent. Stronger gas-melt coupling favors highly explosive …
and magma decouple during ascent. Stronger gas-melt coupling favors highly explosive …
[HTML][HTML] Oxidation of magmas during gain and loss of H2O recorded by trace elements in zircon
RR Loucks, ML Fiorentini - Earth and Planetary Science Letters, 2023 - Elsevier
Hydroxylation-oxidation reactions of the type H 2 O+ Fe→ 2+ Fe 3++ OH−+ 1/2 H 2 oxidise
Fe 2+ in olivine and pyroxenes in oceanic lithosphere prior to subduction and in the supra …
Fe 2+ in olivine and pyroxenes in oceanic lithosphere prior to subduction and in the supra …
Transition between fragmentation and permeable outgassing of low viscosity magmas
Explosive volcanic eruption requires that magma fragments into discrete parcels. Silicic
magma can fragment through brittle failure or other processes that depend on the …
magma can fragment through brittle failure or other processes that depend on the …
The effects of outgassing on the transition between effusive and explosive silicic eruptions
W Degruyter, O Bachmann, A Burgisser… - Earth and Planetary …, 2012 - Elsevier
The eruption style of silicic magmas is affected by the loss of gas (outgassing) during ascent.
We investigate outgassing using a numerical model for one-dimensional, two-phase, steady …
We investigate outgassing using a numerical model for one-dimensional, two-phase, steady …
Deformation experiments of bubble‐and crystal‐bearing magmas: Rheological and microstructural analysis
Simple shear deformation experiments on three‐phase, hydrous, haplogranitic magmas,
composed of quartz crystals (24–65 vol.%), CO2‐rich gas bubbles (9–12 vol.%) and melt in …
composed of quartz crystals (24–65 vol.%), CO2‐rich gas bubbles (9–12 vol.%) and melt in …