Open-vent volcanoes fuelled by depth-integrated magma degassing

M Edmonds, EJ Liu, KV Cashman - Bulletin of Volcanology, 2022 - Springer
Open-vent, persistently degassing volcanoes—such as Stromboli and Etna (Italy), Villarrica
(Chile), Bagana and Manam (Papua New Guinea), Fuego and Pacaya (Guatemala) …

Sulfur degassing from volcanoes: source conditions, surveillance, plume chemistry and earth system impacts

C Oppenheimer, B Scaillet… - Reviews in mineralogy …, 2011 - pubs.geoscienceworld.org
Despite its relatively minor abundance in magmas (compared with H2O and CO2), sulfur
degassing from volcanoes is of tremendous significance. It can exert substantial influence …

Post-entrapment modification of volatiles and oxygen fugacity in olivine-hosted melt inclusions

CE Bucholz, GA Gaetani, MD Behn… - Earth and Planetary …, 2013 - Elsevier
The solubilities of volatiles (H 2 O, CO 2, S, F, and Cl) in basaltic melts are dependent on
variables such as temperature, pressure, melt composition, and redox state. Accordingly …

Exceptional eruptive CO2 emissions from intra-plate alkaline magmatism in the Canary volcanic archipelago

M Burton, A Aiuppa, P Allard… - … Earth & Environment, 2023 - nature.com
Alkaline mafic magmas forming intra-plate oceanic islands are believed to be strongly
enriched in CO2 due to low-degree partial melting of enriched mantle sources. However …

Turmoil at Turrialba Volcano (Costa Rica): Degassing and eruptive processes inferred from high‐frequency gas monitoring

JM de Moor, A Aiuppa, G Avard… - Journal of …, 2016 - Wiley Online Library
Abstract Eruptive activity at Turrialba Volcano (Costa Rica) has escalated significantly since
2014, causing airport and school closures in the capital city of San José. Whether or not new …

Structural control and genesis of the Oligocene Zhenyuan orogenic gold deposit, SW China

J Deng, Q Wang, G Li, Y Zhao - Ore Geology Reviews, 2015 - Elsevier
The Zhenyuan gold deposit with> 50 t gold reserve is located within the Jinshajiang–
Ailaoshan suture zone that formed through the closure of Paleo-Tethyan ocean in late …

Tracking the changing oxidation state of Erebus magmas, from mantle to surface, driven by magma ascent and degassing

Y Moussallam, C Oppenheimer, B Scaillet… - Earth and Planetary …, 2014 - Elsevier
The conventional view holds that the oxidation state of a mantle-derived degassed magma
reflects its source. During magma ascent and degassing the oxidation state is thought to …

Simulating the behavior of volatiles belonging to the C–O–H–S system in silicate melts under magmatic conditions with the software D-Compress

A Burgisser, M Alletti, B Scaillet - Computers & Geosciences, 2015 - Elsevier
Modeling magmatic degassing, or how the volatile distribution between gas and melt
changes at pressure varies, is a complex task that involves a large number of …

[HTML][HTML] CO2, carbonate-rich melts, and brines in the mantle

ML Frezzotti, JLR Touret - Geoscience Frontiers, 2014 - Elsevier
This paper reviews the origin and evolution of fluid inclusions in ultramafic xenoliths,
providing a framework for interpreting the chemistry of mantle fluids in the different …

A CO2‐gas precursor to the March 2015 Villarrica volcano eruption

A Aiuppa, M Bitetto, V Francofonte… - Geochemistry …, 2017 - Wiley Online Library
We present here the first volcanic gas compositional time‐series taken prior to a paroxysmal
eruption of Villarrica volcano (Chile). Our gas plume observations were obtained using a …