Abstract
The oxygen isotopic composition of Archean orthogneisses and charnockites from Southern India is rather uniform (δ18O generally 6-8‰) for metamorphic grades ranging from amphibolite to high-P granulite. Some high-P granulites have high δ18O (~10‰) suggesting sediment contributions. CO2 metamorphism does not appear to have affected the δ18O values of Indian charnockites. -Authors
| Original language | English |
|---|---|
| Pages (from-to) | 282-284 |
| Number of pages | 3 |
| Journal | Journal - Geological Society of India |
| Volume | 34 |
| Issue number | 3 |
| Publication status | Published - 1989 |
| Externally published | Yes |