The Anomalous Seismic Behavior of Aqueous Fluids Released during Dehydration of Chlorite in Subduction Zones

Dehydration and fluid circulation are integral parts of subduction tectonics that govern the dynamics of the wedge mantle. The knowledge of the elastic behavior of aqueous fluid is crucial to understand the fluid–rock interactions in the mantle through velocity profiles. In this study, we investigat...

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Main Authors: Geeth Manthilake, Julien Chantel, Nicolas Guignot, Andrew King
Format: Article
Language:English
Published: MDPI AG 2021-01-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/11/1/70
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author Geeth Manthilake
Julien Chantel
Nicolas Guignot
Andrew King
author_facet Geeth Manthilake
Julien Chantel
Nicolas Guignot
Andrew King
author_sort Geeth Manthilake
collection DOAJ
description Dehydration and fluid circulation are integral parts of subduction tectonics that govern the dynamics of the wedge mantle. The knowledge of the elastic behavior of aqueous fluid is crucial to understand the fluid–rock interactions in the mantle through velocity profiles. In this study, we investigated the elastic wave velocities of chlorite at high pressure beyond its dehydrating temperature, simulating the progressive dehydration of hydrous minerals in subduction zones. The dehydration resulted in an 8% increase in compressional (Vp) and a 5% decrease in shear wave (Vs) velocities at 950 K. The increase in Vp can be attributed to the stiffening of the sample due to the formation of secondary mineral phases followed by the dehydration of chlorite. The fluid-bearing samples exhibited Vp/Vs of 2.45 at 950 K. These seismic parameters are notably different from the major mantle minerals or hydrous silicate melts and provide unique seismic criteria for detecting mantle fluids through seismic tomography.
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spelling doaj.art-f7b64427c3894e83beda68c170f1662c2023-12-03T13:01:53ZengMDPI AGMinerals2075-163X2021-01-011117010.3390/min11010070The Anomalous Seismic Behavior of Aqueous Fluids Released during Dehydration of Chlorite in Subduction ZonesGeeth Manthilake0Julien Chantel1Nicolas Guignot2Andrew King3Laboratoire Magmas et Volcans, Université Clermont Auvergne, CNRS, IRD, OPGC, 63000 Clermont-Ferrand, FranceUniversity Lille, CNRS, INRAE, Centrale Lille, UMR 8207—UMET—Unité Matériaux et Transformations, 59000 Lille, FranceSynchrotron SOLEIL, 91192 Gif-Sur-Yvette, FranceSynchrotron SOLEIL, 91192 Gif-Sur-Yvette, FranceDehydration and fluid circulation are integral parts of subduction tectonics that govern the dynamics of the wedge mantle. The knowledge of the elastic behavior of aqueous fluid is crucial to understand the fluid–rock interactions in the mantle through velocity profiles. In this study, we investigated the elastic wave velocities of chlorite at high pressure beyond its dehydrating temperature, simulating the progressive dehydration of hydrous minerals in subduction zones. The dehydration resulted in an 8% increase in compressional (Vp) and a 5% decrease in shear wave (Vs) velocities at 950 K. The increase in Vp can be attributed to the stiffening of the sample due to the formation of secondary mineral phases followed by the dehydration of chlorite. The fluid-bearing samples exhibited Vp/Vs of 2.45 at 950 K. These seismic parameters are notably different from the major mantle minerals or hydrous silicate melts and provide unique seismic criteria for detecting mantle fluids through seismic tomography.https://www.mdpi.com/2075-163X/11/1/70elastic wave velocitysubduction zonedehydrationchloriteseismic anomalieshigh pressure
spellingShingle Geeth Manthilake
Julien Chantel
Nicolas Guignot
Andrew King
The Anomalous Seismic Behavior of Aqueous Fluids Released during Dehydration of Chlorite in Subduction Zones
Minerals
elastic wave velocity
subduction zone
dehydration
chlorite
seismic anomalies
high pressure
title The Anomalous Seismic Behavior of Aqueous Fluids Released during Dehydration of Chlorite in Subduction Zones
title_full The Anomalous Seismic Behavior of Aqueous Fluids Released during Dehydration of Chlorite in Subduction Zones
title_fullStr The Anomalous Seismic Behavior of Aqueous Fluids Released during Dehydration of Chlorite in Subduction Zones
title_full_unstemmed The Anomalous Seismic Behavior of Aqueous Fluids Released during Dehydration of Chlorite in Subduction Zones
title_short The Anomalous Seismic Behavior of Aqueous Fluids Released during Dehydration of Chlorite in Subduction Zones
title_sort anomalous seismic behavior of aqueous fluids released during dehydration of chlorite in subduction zones
topic elastic wave velocity
subduction zone
dehydration
chlorite
seismic anomalies
high pressure
url https://www.mdpi.com/2075-163X/11/1/70
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