The redox state of Earth's convecting mantle, masked by the lithospheric plates and basaltic magmatism of plate tectonics, is a key unknown in the evolutionary history of our planet …
DA Neave, KD Putirka - American Mineralogist, 2017 - degruyter.com
Pressure is one of the key variables that controls magmatic phase equilibria. However, estimating magma storage pressures from erupted products can be challenging. Various …
P Segall - … Transactions of the Royal Society A, 2019 - royalsocietypublishing.org
Geodetic observations on volcanoes can reveal important aspects of crustal magma chambers. The rate of decay of deformation with distance reflects the centroid depth of the …
Deformation of the ground surface at active volcanoes provides information about magma movements at depth. Improved seafloor deformation measurements between 2011 and …
Moving beyond the widely used kinematic models for the deformation sources, we present a new dynamic model to describe the process of injecting magma into an existing magma …
P Segall - Journal of Geophysical Research: Solid Earth, 2016 - Wiley Online Library
I analyze an approximate solution for spherical magma chambers (radius R1) surrounded by Maxwell viscoelastic shells (radius R2) in elastic half‐spaces following a sudden decrease …
M Townsend - Earth and Planetary Science Letters, 2022 - Elsevier
Surface deformation at active volcanoes reflects a wide variety of magmatic and crustal processes, and the typical kinematic models employed to interpret these geodetic data are …
Large volume effusive eruptions with relatively minor observed precursory signals are at odds with widely used models to interpret volcano deformation. Here we propose a new …
P Lundgren, T Girona, MG Bato, VJ Realmuto… - Scientific reports, 2020 - nature.com
Silicic magmatic systems are the most dangerous volcanoes on Earth, capable of large and catastrophic eruptions, yet their low eruptive frequency makes it challenging to interpret their …