Magma transport and storage at Piton de La Fournaise (La Réunion) between 1972 and 2007: A review of geophysical and geochemical data

A Peltier, P Bachèlery, T Staudacher - Journal of Volcanology and …, 2009 - Elsevier
Since the middle of the 20th century, improvement in volcano monitoring techniques has
provided large data sets that can be used to evaluate the evolution of magma plumbing …

Rift zones and magma plumbing system of Piton de la Fournaise volcano: How do they differ from Hawaii and Etna?

L Michon, V Ferrazzini, A Di Muro, N Villeneuve… - Journal of Volcanology …, 2015 - Elsevier
On ocean basaltic volcanoes, magma transfer to the surface proceeds by subvertical ascent
from the mantle lithosphere through the oceanic crust and the volcanic edifice, possibly …

Solubility of H2O-and CO2-bearing fluids in tholeiitic basalts at pressures up to 500 MPa

TA Shishkina, RE Botcharnikov, F Holtz, RR Almeev… - Chemical geology, 2010 - Elsevier
The solubility of H2O-and CO2-bearing fluids in tholeiitic basalts has been investigated
experimentally at temperature of 1250° C and pressures of 50, 100, 200, 300, 400 and …

Dendritic crystallization: a single process for all the textures of olivine in basalts?

B Welsch, F Faure, V Famin, A Baronnet… - Journal of …, 2013 - academic.oup.com
The olivine macrocrysts found in oceanites, picrites and magnesian basalts erupted at
hotspot volcanoes are generally interpreted either as phenocrysts crystallized from the …

The shallow plumbing system of Piton de la Fournaise Volcano (La Reunion Island, Indian Ocean) revealed by the major 2007 caldera-forming eruption

A Di Muro, N Métrich, D Vergani, M Rosi… - Journal of …, 2014 - academic.oup.com
The 2007 caldera-forming eruption of Piton de la Fournaise (PdF) erupted the largest
volume of magma (210 Mm3) recorded at this volcano in at least three centuries. Major and …

Extensive CO2 degassing in the upper mantle beneath oceanic basaltic volcanoes: First insights from Piton de la Fournaise volcano (La Réunion Island)

G Boudoire, AL Rizzo, A Di Muro, F Grassa… - … et Cosmochimica Acta, 2018 - Elsevier
In spite of its major role on the atmospheric volatile budget, climate, and tracking magmatic
transfers, mantle (CO 2) degassing below volcanoes is still poorly understood. Most of the …

The mantle source of basalts from Reunion Island is not more oxidized than the MORB source mantle

M Brounce, E Stolper, J Eiler - Contributions to Mineralogy and Petrology, 2022 - Springer
Glasses quenched from relatively undegassed ocean island magmas erupted from
volcanoes at Iceland, Hawaii, the Canary Islands, and Erebus have elevated Fe 3+/∑ Fe …

Upper mantle mush zones beneath low melt flux ocean island volcanoes: insights from Isla Floreana, Galápagos

MLM Gleeson, SA Gibson, MJ Stock - Journal of Petrology, 2020 - academic.oup.com
The physicochemical characteristics of sub-volcanic magma storage regions have important
implications for magma system dynamics and pre-eruptive behaviour. The architecture of …

Integrating field, textural, and geochemical monitoring to track eruption triggers and dynamics: a case study from Piton de la Fournaise

L Gurioli, A Di Muro, I Vlastélic, S Moune, S Thivet… - Solid Earth, 2018 - se.copernicus.org
The 2014 eruption at Piton de la Fournaise (PdF), La Réunion, which occurred after 41
months of quiescence, began with surprisingly little precursory activity and was one of the …

Two magma bodies beneath the summit of Kīlauea Volcano unveiled by isotopically distinct melt deliveries from the mantle

AJ Pietruszka, DE Heaton, JP Marske… - Earth and Planetary …, 2015 - Elsevier
The summit magma storage reservoir of Kīlauea Volcano is one of the most important
components of the magmatic plumbing system of this frequently active basaltic shield …