Results 21 to 30 of about 418,217 (192)

Large mantle magma reservoir of Afar, Ethopia [PDF]

open access: yesFrontiers in Earth Science, 2014
Artículo de COMENTARIO GENERAL Front. Earth Sci., 16 de abril de 2014Sec.
Afroz Ahmad eShah
doaj   +3 more sources

Coupled subdaily and multiweek cycles during the lava dome eruption of Soufriere Hills Volcano, Montserrat [PDF]

open access: yes, 2013
Observations of volcanoes extruding andesitic lava to produce lava domes often reveal cyclic behaviour. At Soufriere Hills Volcano, Montserrat, cycles with sub-daily and multi-week periods have been recognised on many occasions.
Costa, A.   +12 more
core   +1 more source

Magma Pathways and Their Interactions Inferred from InSAR and Stress Modeling at Nyamulagira Volcano, D.R. Congo

open access: yesRemote Sensing, 2015
A summit and upper flank eruption occurred at Nyamulagira volcano, Democratic Republic of Congo, from 2–27 January 2010. Eruptions at Nyamulagira during 1996–2010 occurred from eruptive fissures on the upper flanks or within the summit caldera and were ...
Christelle Wauthier   +4 more
doaj   +1 more source

Vault-housed extensometers recorded a rapid initial pulse before precursory magma reservoir inflation related to the 2011 eruption of Shinmoe-dake, Japan

open access: yesEarth, Planets and Space, 2020
Previous studies of the major eruption at Shinmoe-dake volcano, Japan, in January 2011 suggested that gradual injection of magma from a deep source into a shallow reservoir began in December 2009 and led to the major eruption.
Ken’ichi Yamazaki   +2 more
doaj   +1 more source

Top–Down Precursory Volcanic Seismicity: Implications for ‘Stealth’ Magma Ascent and Long-Term Eruption Forecasting

open access: yesFrontiers in Earth Science, 2018
Volcanic eruptions occur when a conduit forms to connect a crustal magma reservoir to Earth’s surface. Conduit formation is generally assumed to be a ‘bottom–up’ process and a major driver of precursory volcanic seismicity, which is the most commonly ...
Diana C. Roman, Katharine V. Cashman
doaj   +1 more source

Temporal magmatic evolution of the Fani Maoré submarine eruption 50 km east of Mayotte revealed by in situ sampling and petrological monitoring

open access: yesComptes Rendus. Géoscience, 2022
The “Fani Maoré” eruption off the coasts of Mayotte has been intensively monitored by applying methods similar to those used for subaerial eruptions. Repeated high-resolution bathymetric surveys and dredging, coupled with petrological analyses of time ...
Berthod, Carole   +30 more
doaj   +1 more source

Unraveling the Physics of the Yellowstone Magmatic System Using Geodynamic Simulations

open access: yesFrontiers in Earth Science, 2018
The Yellowstone magmatic system is one of the largest magmatic systems on Earth, and thus an ideal location to study magmatic processes. Whereas previous seismic tomography results could only image a shallow magma reservoir, a recent study using more ...
Georg S. Reuber   +5 more
doaj   +1 more source

Gabbroic enclave in intermediate ignimbrites: The youngest eruptive event in the northern Luzon Arc-Taiwan region

open access: yesTerrestrial, Atmospheric and Oceanic Sciences, 2021
The white ignimbrite layer on top of volcanic sequences in the Coastal Range is the youngest eruption of the northern Luzon Arc in the Taiwan region. A gabbroic enclave was coexisting with the andesitic ignimbrite in this sequence. This study reports the
Yu-Ming Lai   +5 more
doaj   +1 more source

Minimum Detectable Mass and Volume Fluxes During Magmatic Recharge at High Prominence Volcanoes: An Application to Erciyes Dağ Volcano (Turkey)

open access: yesFrontiers in Earth Science, 2021
Magma reservoir recharge is widely recognised as a precursor of eruptive activity. However, the causative relationships between reservoir rejuvenation and surface observables such as gravitational potential field changes and ground deformation are still ...
Katie Males, Jo Gottsmann, Jo Gottsmann
doaj   +1 more source

Imaging a magma plumbing system from MASH zone to magma reservoir [PDF]

open access: yesEarth and Planetary Science Letters, 2017
The Puna Plateau of the Central Andes is a well-suited location to investigate the processes associated with the tectono-magmatic development of a Cordilleran system. These processes include long-lived subduction (including shallow and steep phases), substantial crustal thickening, the emplacement of large volumes of igneous rocks, and probably ...
Jonathan R. Delph   +4 more
openaire   +3 more sources

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