Timescales of interface-coupled dissolution-precipitation reactions on carbonates

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Timescales of interface-coupled dissolution-precipitation reactions on carbonates

In the Earth's upper crust, where aqueous fluids can circulate freely, most mineral transformations are controlled by the coupling between the dissolution of a mineral that releases chemical species into the fluid and precipitation of new minerals that contain some of the released species in th...

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Bibliographic Details
Main Authors:	Renard, F., Røyne, A., Putnis, Christine
Format:	Journal Article
Published:	Elsevier 2019
Online Access:	http://creativecommons.org/licenses/by-nc-nd/4.0/ http://hdl.handle.net/20.500.11937/67491

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