| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4721932 | Physics and Chemistry of the Earth, Parts A/B/C | 2007 | 14 Pages |
Abstract
The comparison of results obtained with powdered and compact solids is only feasible for short time experiments. Aqueous chemistry and solid analyses indicate the dissolution of pyrite, dolomite and organic carbon with the precipitation of calcite. Precipitations of zeolites and K-feldspars occur sometimes and are only evidenced by SEM analyses. Nevertheless, silicates dissolution or precipitation is unclear through XRD analyses. Experimental conditions influence widely the intensity/nature of processes and prevent the transposition of data obtained in given conditions to other ones.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
I. Devol-Brown, E. Tinseau, D. Bartier, A. Mifsud, D. Stammose,
