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...
| Main Authors: | , , |
|---|---|
| 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 |