Vesiculation of Rhyolitic Melts Under Oscillatory Pressure

Vesiculation of Rhyolitic Melts Under Oscillatory Pressure

Magma ascending in the Earth’s crust can undergo oscillations in pressure, from ultra-low frequency changes associated with tectonics, to relatively higher frequency oscillations associated with seismicity. Seismic waves travelling through shallow magma bodies can lead to a range of unrest phenomena...

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Bibliographic Details
Main Authors: Gilles Seropian, Ben M. Kennedy, Jackie E. Kendrick, Yan Lavallée, Alexander R. L. Nichols, Felix W. von Aulock, Donald B. Dingwell, Kai-Uwe Hess, Anthony Lamur, Jenny Schauroth, Jérémie Vasseur, Fabian B. Wadsworth
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-03-01
Series:Frontiers in Earth Science
Subjects:
vesiculation
bubbles
pressure oscillations
rhyolite
high temperature
experimental
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2022.812311/full

Internet

https://www.frontiersin.org/articles/10.3389/feart.2022.812311/full

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