Fluid Pressure Changes Recorded by Trace Elements in Quartz

Abstract Fluid pressure is a key parameter in earthquake mechanics, controlling seismic failure and plate coupling in convergent zones. Yet fluid pressure is also extremely difficult to quantify at seismogenic depth, which limits our knowledge of the stress state in accretionary prisms. Here, we sho...

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Bibliographic Details
Published in:	Geochemistry, Geophysics, Geosystems
Main Authors:	Hugues Raimbourg, Vincent Famin, Aurélien Canizarès, Emmanuel Le Trong
Format:	Article
Language:	English
Published:	Wiley 2022-10-01
Subjects:	quartz geochemistry earthquakes fluids trace elements
Online Access:	https://doi.org/10.1029/2022GC010346

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