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| Content Provider | Springer Nature Link |
|---|---|
| Author | Hergt, Janet |
| Copyright Year | 2000 |
| Abstract | O values, the magmas retain initial 87Sr/86Sr Compositions of greater than 0.709 (e.g. Hoefs et al. 1980). Consistent with this is the lack of a radiogenic Os isotope signature in these rocks (e.g. Molzahn et al. 1996) as would be expected with assimilation of continental crust. Comments here are not concerned with the AFC calculations employed to describe the variations within the suite of samples from the Prince Albert mountains studied by Antonini et al., but rather, the extrapolation of these to more primitive compositions.Antonini et al. have revived the possibility that the unusual chemical features of the least evolved low Ti continental flood basalts of the Ferrar Province reflect a crustal-level interplay between mantle-derived magmas and the continental crust. It is argued here that they have not demonstrated their claim. |
| Starting Page | 240 |
| Ending Page | 244 |
| Page Count | 5 |
| File Format | |
| ISSN | 00107999 |
| Journal | Contributions to Mineralogy and Petrology |
| Volume Number | 139 |
| Issue Number | 2 |
| e-ISSN | 14320967 |
| Language | English |
| Publisher | Springer-Verlag |
| Publisher Date | 2000-06-06 |
| Publisher Place | Berlin/Heidelberg |
| Access Restriction | One Nation One Subscription (ONOS) |
| Content Type | Text |
| Resource Type | Article |
| Subject | Geochemistry and Petrology Geophysics |
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