Generating porosity during olivine carbonation via dissolution channels and expansion cracks

<p>The olivine carbonation reaction, in which carbon dioxide is chemically incorporated to form carbonate, is central to the emerging carbon sequestration method using ultramafic rocks. The rate of this retrograde metamorphic reaction is controlled, in part, by the available reactive surfa...

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Bibliographic Details
Main Authors: T. Xing, W. Zhu, F. Fusseis, H. Lisabeth
Format: Article
Language:English
Published: Copernicus Publications 2018-07-01
Series:Solid Earth
Online Access:https://www.solid-earth.net/9/879/2018/se-9-879-2018.pdf