Low Temperature Serpentinite Replacement by Carbonates during Seawater Influx in the Newfoundland Margin

Low Temperature Serpentinite Replacement by Carbonates during Seawater Influx in the Newfoundland Margin

Serpentinite replacement by carbonates in the seafloor is one of the main carbonation processes in nature providing insights into the mechanisms of CO<sub>2</sub> sequestration; however, the onset of this process and the conditions for the reaction to occur are not yet fully understood....

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Bibliographic Details
Main Authors: Suzanne Picazo, Benjamin Malvoisin, Lukas Baumgartner, Anne-Sophie Bouvier
Format: Article
Language:English
Published: MDPI AG 2020-02-01
Series:Minerals
Subjects:
carbonation
co<sub>2</sub> sequestration
replacement process
low temperature carbonate precipitation
secondary ion mass spectrometer
seawater influx
hydrothermal circulation
ophicalcite
Online Access:https://www.mdpi.com/2075-163X/10/2/184

Internet

https://www.mdpi.com/2075-163X/10/2/184

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