Volcanological evolution of Montagne Pelée (Martinique): A textbook case of alternating Plinian and dome-forming eruptions
G Boudon, H Balcone-Boissard - Earth-Science Reviews, 2021 - Elsevier
Montagne Pelée is one of the most active volcanoes of the Lesser Antilles arc, with two to
three magmatic eruptions per millennium and an estimated magmatic production rate in the …
three magmatic eruptions per millennium and an estimated magmatic production rate in the …
Growth process of the lava dome/flow complex at Sinabung Volcano during 2013–2016
Abstract Mount Sinabung, North Sumatra, Indonesia, erupted for the first time in 2010 and
reactivated again in 2013. The eruption started with a phreatic phase, changed to …
reactivated again in 2013. The eruption started with a phreatic phase, changed to …
[HTML][HTML] Gas and ash emissions associated with the 2010–present activity of Sinabung Volcano, Indonesia
Abstract Sinabung Volcano (Sumatra, Indonesia) awoke from over 1200 years of dormancy
with multiple phreatic explosions in 2010. After a period of quiescence, Sinabung activity …
with multiple phreatic explosions in 2010. After a period of quiescence, Sinabung activity …
Petrological evidence of rapid evolution of the magma plumbing system of Bezymianny volcano in Kamchatka before the December 20th, 2017 eruption
We used petrological data on samples of the December 20th, 2017 eruption of the
Bezymianny volcano (Kamchatka, Russia) to investigate the evolution of the magmatic …
Bezymianny volcano (Kamchatka, Russia) to investigate the evolution of the magmatic …
Vapor-phase cristobalite as a durable indicator of magmatic pore structure and halogen degassing: an example from White Island volcano (New Zealand)
C Ian Schipper, C Mandon, A Maksimenko… - Bulletin of …, 2017 - Springer
Vesicles in volcanic rocks are physical records of magmatic degassing; however, the
interpretation of their textures is complicated by resorption, coalescence, and collapse. We …
interpretation of their textures is complicated by resorption, coalescence, and collapse. We …
Vapor-phase crystallization from a hydrous silicate melt: an experimental simulation of diktytaxitic texture
Groundmass textures of volcanic rocks provide valuable insights into the processes of
magma ascent, crystallization, and eruption. The diktytaxitic texture, characterized by a lath …
magma ascent, crystallization, and eruption. The diktytaxitic texture, characterized by a lath …
3D electrical imaging of the inner structure of a complex lava dome, Puy de Dôme volcano (French Massif Central, France)
Lava domes result from extrusion of massive lava, frequent explosions and collapses. This
contribution focuses on a complex trachytic lava dome, the Puy de Dôme volcano, located in …
contribution focuses on a complex trachytic lava dome, the Puy de Dôme volcano, located in …
[HTML][HTML] Pre-eruptive conditions at satellite vent eruptions at Teide-Pico Viejo complex (Tenerife, Canary Islands)
Abstract The Teide-Pico Viejo (T-PV) stratovolcanoes constitute one of the most potentially
active volcanic complexes in Europe. T-PV was traditionally considered as a non-explosive …
active volcanic complexes in Europe. T-PV was traditionally considered as a non-explosive …
Evolution of monogenetic rift-related alkaline magmatism in south Egypt: insight from stratigraphy, geochronology, and geochemistry of the Natash volcanics
EEDAH Khalaf, T Sano, Y Tsutsumi - Journal of African Earth Sciences, 2018 - Elsevier
Abstract The Mesozoic Natash volcanics are rift-related monogenetic volcanic complex that
erupted in south Eastern Desert of Egypt. The architecture of their building has evolved …
erupted in south Eastern Desert of Egypt. The architecture of their building has evolved …
Rheological change and degassing during a trachytic Vulcanian eruption at Kilian Volcano, Chaîne des Puys, France
Magma ascent during silicic dome-forming eruptions is characterized by significant changes
in magma viscosity, permeability, and gas overpressure in the conduit. These changes …
in magma viscosity, permeability, and gas overpressure in the conduit. These changes …