Results 81 to 90 of about 392,695 (199)
Megacrystals track magma convection between reservoir and surface [PDF]
International audienceActive volcanoes are typically fed by magmatic reservoirs situated within the upper crust. The development of thermal and/or compositional gradients in such magma chambers may lead to vigorous convection as inferred from theoretical
Kimball, Christine +10 more
core +2 more sources
The architecture of magma plumbing systems plays a fundamental role in volcano eruption and evolution. However, the precise configuration of crustal magma reservoirs and conduits responsible for supplying eruptions are difficult to explore across most ...
Jidong Yang +8 more
doaj +1 more source
Abstract Megathrust slip behavior in subduction zones can vary along‐strike, yet the mechanisms driving this variability remain uncertain. The Middle America trench offshore Mexico provides an ideal setting to investigate the structural controls on megathrust slip behavior.
Davis Hagemeier +10 more
wiley +1 more source
International audiencePressure variations in a magma reservoir may cause deformation at the surface and a redistribution of the stress in the surrounding rock.
Gargani, Julien
core +1 more source
Geofluid mapping reveals the connection between magmas, fluids, and earthquakes
Subsurface geofluids drive Earth’s evolution through seismogenesis, volcanism, and plate motion. Previous geofluid-distribution estimates from various geophysical methods show large variations.
Hikaru Iwamori +8 more
doaj +1 more source
Implications of Thermal Weakening and Magma Compressibility for Volcano Monitoring
Abstract Magmatic intrusion and volcanic deformation are traditionally approximated with an inflating cavity in an elastic halfspace. Various analytical models predict surface displacement as a function of pressure or volume change, depth, and elastic crustal properties.
A. Spang +4 more
wiley +1 more source
Lava production at Soufriere Hills Volcano, Montserrat: 1995-2009 [PDF]
[1] We estimate that about 1 km3 of andesitic lava has been produced at Soufrière Hills Volcano, Montserrat from 1995 to 2009. There were three major episodes of extrusion, each lasting about 2 to 3.5 years and producing about 280 to 340 M m3 of lava ...
Calder, E. S. +14 more
core +1 more source
Thermo‐Mechanical Controls on Central‐Vent Caldera Collapse
Abstract Large‐scale magmatic systems are associated with catastrophic caldera‐forming eruptions, posing hazards to millions near active volcanoes. Despite occurring across a range of sizes, the physics driving caldera collapse remain incompletely understood. While large calderas have received considerable attention, moderately sized calderas (∼5–10 km)
Pascal S. Aellig +2 more
wiley +1 more source
Measurements of volcano deformation are increasingly routine, but constraining complex magma reservoir geometries via inversions of surface deformation measurements remains challenging.
Taiyi A. Wang +2 more
doaj +1 more source
Role of mechanical erosion in controlling the effusion rate of basaltic eruptions
In many basaltic eruptions, observations show that the effusion rate of magma has a typical dependence on time: the effusion rate curves show first a period of increasing and later a decreasing phase by a maximum value. We present a model to explain this
Antonello Piombo +2 more
doaj +1 more source

