Results 31 to 40 of about 1,472 (257)

Crystal Shape Control on the Repacking and Jamming of Crystal‐Rich Mushes

open access: yesGeophysical Research Letters, 2022
AbstractThe rheology of crustal mushes is a crucial parameter controlling melt segregation and magma flow. However, the relations between mush dynamics and crystal size and shape distribution remain poorly understood because of the complexity of melt‐crystal and crystal‐crystal interactions.
Susana Hoyos   +3 more
openaire   +1 more source

Mush Amalgamation, Short Residence, and Sparse Detectability of Eruptible Magma Before Andean Super‐Eruptions

open access: yesGeochemistry, Geophysics, Geosystems, 2023
Giant volcanic eruptions have the potential to overturn civilizations. Yet, the driving mechanism and timescale over which batholithic magma reservoirs transition from non‐eruptible crystal mush to mobile melt‐dominated stages and our capacity to detect ...
G. Weber, J. Blundy, D. Bevan
doaj   +1 more source

Progressive underplating of mafic material at mid-crustal depth beneath Ischia volcano, Italy

open access: yesCommunications Earth & Environment, 2023
The destructive (Mw 3.9) earthquake of 21 August 2017 re-opened the question on where magma resides at the Ischia island volcano. The peculiar complexity of the seismic source initiated the debate on the involvement of fluid-related processes, but the ...
Irene Bianchi   +3 more
doaj   +1 more source

Time scales of crystal mixing in magma mushes [PDF]

open access: yesGeophysical Research Letters, 2016
AbstractMagma mixing is widely recognized as a means of producing compositional diversity and preconditioning magmas for eruption. However, the processes and associated time scales that produce the commonly observed expressions of magma mixing are poorly understood, especially under crystal‐rich conditions.
Schleicher, Jillian M.   +3 more
openaire   +3 more sources

A Crystal Mush Perspective Explains Magma Variability at La Fossa Volcano (Vulcano, Italy) [PDF]

open access: yes, 2021
The eruptive products of the last 1000 years at La Fossa volcano on the island of Vulcano (Italy) are characterized by abrupt changes of chemical composition that span from latite to rhyolite.
Anna Gioncada   +3 more
core   +2 more sources

The Role of Crystal Accumulation and Cumulate Remobilization in the Formation of Large Zoned Ignimbrites: Insights From the Aso-4 Caldera-forming Eruption, Kyushu, Japan

open access: yesFrontiers in Earth Science, 2021
The Aso-4 caldera-forming event (86.4 ± 1.1 ka, VEI-8) is the second largest volcanic eruption Earth experienced in the past 100 ka. The ignimbrite sheets produced during this event are some of the first ever described compositionally zoned pyroclastic ...
Franziska Keller   +3 more
doaj   +1 more source

The permeability of magma mush [PDF]

open access: yes, 2023
Models for the evolution of magma mush zones are of fundamental importance for understanding magma storage, differentiation in the crust, and melt extraction processes that prime eruptions.
BRETAGNE, ELOISE,MARIE
core  

Interfacial growth morphologies in dense eutectic crystal mushes

open access: yesIMA Journal of Applied Mathematics, 2023
Abstract We consider the interfacial growth morphologies of crystals growing in contact in crystal mushes, with a specific application to those formed by the solidification of basaltic magma. We focus on the particular case of an augite (pyroxene) crystal growing between two plagioclase crystals.
Fowler, Andrew, Holness, Marian B.
openaire   +3 more sources

Time scales of open-system processes in a complex and heterogeneous mush-dominated plumbing system

open access: yes, 2022
The architecture of a mush-dominated plumbing system in active volcanic areas conditions the magma pathways feeding eruptions. Open-system processes along these pathways and the associated time scales are directly related to monitoring data and eruptive
Marani, Michael P.   +6 more
core   +3 more sources

Defining Pre-eruptive Conditions of the Havre 2012 Submarine Rhyolite Eruption Using Crystal Archives

open access: yesFrontiers in Earth Science, 2020
The 2012 Havre eruption evacuated a crystal-poor rhyolite (∼3–7% crystals) producing a volumetrically dominant (∼1.4 km3) pumice raft, as well as seafloor giant pumice (5–8%) and lavas (12–14%) at the vent (∼0.1 km3), both of which have subtly higher ...
Joseph Knafelc   +3 more
doaj   +1 more source

Home - About - Disclaimer - Privacy