| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4699641 | Chemical Geology | 2011 | 13 Pages |
Abstract
⺠δ18O of wollastonite rims record disequilibrium between reactants and products. ⺠We model δ18O using a mass balance approach, based on the wollastonite-forming reaction. ⺠This model successfully reproduces many measured δ18O values of wollastonite rims.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Susanne Skora, Lukas P. Baumgartner, Torsten W. Vennemann,