Experimental evidence of pressure effects on spinel dissolution and peridotite serpentinization kinetics under shallow hydrothermal conditions

Experimental evidence of pressure effects on spinel dissolution and peridotite serpentinization kinetics under shallow hydrothermal conditions

Serpentinization reactions are paramount to understand hydro-geothermal activity near plate boundaries and mafic–ultramafic massifs, as well as fluid and element transfer between the Earth’s mantle and crust. However, fluid-rock element exchange and serpentinization kinetics under shallow hydrotherm...

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Bibliographic Details
Main Authors: Yuri de Melo Portella, Rommulo Vieira Conceição, Tiago Abreu Siqueira, Lucas Bonan Gomes, Rodrigo Sebastian Iglesias
Format: Article
Language:English
Published: Elsevier 2024-03-01
Series:Geoscience Frontiers
Subjects:
Serpentine
Volume expansion
Serpentinization fluids
Lost City hydrothermal field
Serpentinite-hosted hydrothermal systems
Hydrogen (H2) generation
Online Access:http://www.sciencedirect.com/science/article/pii/S167498712300230X

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http://www.sciencedirect.com/science/article/pii/S167498712300230X

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