AGU Centennial Grand Challenge: Volcanoes and Deep Carbon Global CO2 Emissions From Subaerial Volcanism—Recent Progress and Future Challenges
TP Fischer, A Aiuppa - Geochemistry, Geophysics, Geosystems, 2020 - Wiley Online Library
Quantifying the global volcanic CO2 output from subaerial volcanism is key for a better
understanding of rates and mechanisms of carbon cycling in and out of our planet and their …
understanding of rates and mechanisms of carbon cycling in and out of our planet and their …
An interpretative view of open-vent volcanoes
S Vergniolle, N Métrich - Bulletin of Volcanology, 2022 - Springer
Open-vent volcanoes are special systems where the dynamics of sustained magmatic
processes can be thoroughly investigated and where new monitoring tools can be tested …
processes can be thoroughly investigated and where new monitoring tools can be tested …
Carbon dioxide emissions from subaerial volcanic regions
Volcanism and metamorphism are the principal geologic processes that drive carbon
transfer from the interior of Earth to the surface reservoir. 1–4 Input of carbon to the surface …
transfer from the interior of Earth to the surface reservoir. 1–4 Input of carbon to the surface …
CO2 flux emissions from the Earth's most actively degassing volcanoes, 2005–2015
The global carbon dioxide (CO2) flux from subaerial volcanoes remains poorly quantified,
limiting our understanding of the deep carbon cycle during geologic time and in modern …
limiting our understanding of the deep carbon cycle during geologic time and in modern …
Continental degassing of helium in an active tectonic setting (northern Italy): the role of seismicity
In order to investigate the variability of helium degassing in continental regions, its release
from rocks and emission into the atmosphere, here we studied the degassing of volatiles in a …
from rocks and emission into the atmosphere, here we studied the degassing of volatiles in a …
Reviewing the geodynamic impact of aseismic ridges subduction on the tectonic-magmatic evolution of the Southern Puna plateau
W Báez, E Bustos, A Chiodi, HPA García… - Journal of South …, 2023 - Elsevier
Abstract The Southern Puna (∼ 24° S to 27° S) is an outstanding segment of the Central
Andes where the subduction of aseismic ridges, multi-scale lithospheric foundering, and the …
Andes where the subduction of aseismic ridges, multi-scale lithospheric foundering, and the …
Geochemistry of Noble Gases and CO2 in Fluid Inclusions From Lithospheric Mantle Beneath Wilcza Góra (Lower Silesia, Southwest Poland)
AL Rizzo, B Pelorosso, M Coltorti, T Ntaflos… - Frontiers in Earth …, 2018 - frontiersin.org
Knowledge of the products originating from the subcontinental lithospheric mantle (SCLM) is
crucial for constraining the geochemical features and evolution of the mantle. This study …
crucial for constraining the geochemical features and evolution of the mantle. This study …
Periodicity in volcanic gas plumes: a review and analysis
Persistent non-explosive passive degassing is a common characteristic of active volcanoes.
Distinct periodic components in measurable parameters of gas release have been widely …
Distinct periodic components in measurable parameters of gas release have been widely …
3He/4He Signature of Magmatic Fluids from Telica (Nicaragua) and Baru (Panama) Volcanoes, Central American Volcanic Arc
Featured Application The use of noble gas isotopic signature of fluid inclusions is
increasingly being applied as a complement to traditional volcanic gas sampling and …
increasingly being applied as a complement to traditional volcanic gas sampling and …
Petrological and noble gas features of Lascar and Lastarria volcanoes (Chile): Inferences on plumbing systems and mantle characteristics
Lascar (5592 m asl) and Lastarria (5697 m asl) are Chilean active stratovolcanoes located
in the Central Volcanic Zone (CVZ; 16° S to 28° S) that have developed on top of a 71 km …
in the Central Volcanic Zone (CVZ; 16° S to 28° S) that have developed on top of a 71 km …