| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6440421 | Lithos | 2016 | 67 Pages |
Abstract
Temperature and fO2 were calculated (950 °C; Îlog fO2 (QFM), â 1.70 to â 0.39) at a fixed pressure of 15 kbar, confirming the tendency of the anhydrous Greene Point xenolith population to have higher equilibration temperatures and comparable redox conditions, compared to the nearby amphibole-bearing peridotites from Baker Rocks.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Beatrice Pelorosso, Costanza Bonadiman, Massimo Coltorti, Barbara Faccini, Massimiliano Melchiorre, Theodoros Ntaflos, Michel Gregoire,