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"The crystals settle out of the magma and what doesn't crystallise is the mugearite magma, which can eventually make its way to the surface as a volcanic eruption".
These include the idea that shockwaves from the quakes can cause mushy semisolid magmas to liquefy into something more likely to erupt, or even that earthquakes can accelerate the growth of bubbles in magma, which can increase magma pressures.
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Events like a new pulse of hot magma into the chamber like that which can precede an eruption can cause elements inside a crystal, such as iron and magnesium, to migrate toward the crystal's core or toward its edges, creating new rings.
Lee et al. (2007) investigated the trace element systematics in natural Fe O S magmas and proposed that a similar Fe O S melt, which can account for the difference between the 142Nd/144Nd ratios of chondrites and the ASE, had formed during the final stages of magma ocean solidification.
Finally, the speed at which gases are released from magma is affected by the number of small crystals, which can act as nucleation sites where gas bubbles begin to form.
The effect could be detected as a heterogeneity in the medium, which can prove the existence of the magma body.
Emplacement of magma or changes in hydrothermal activity affect the resistivity structure beneath volcanoes, which can be monitored by electromagnetic surveys.
Research has also revealed that the ridge crests are characterized by anomalously low seismic wave velocities, which can be attributed to thermal expansion and microfracturing associated with the upwelling magma.
Aftershocks were distributed avoiding the LVZ beneath Onikobe Caldera, which can be explained by material softening under very high temperature of molten magma.
The occurrence of inflation episodes due to magma upraising or hydro-thermal fluid circulation can be the cause for significant volume and rock physical property changes which can produce density variations detectable by cosmic ray muon radiography.
JohnO hired me, because I once bought a used Can CD, and I was able to have a coherent conversation about Magma, which made for an entertaining interview.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com