| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6442176 | Precambrian Research | 2016 | 69 Pages |
Abstract
The economic deposits of Fe-Ti associated with retro-eclogitic and ultramafic members of the FMUC and enclosed within the late Ediacaran granite can be linked in part by early accumulation under magmatic conditions, secondary enrichment of rutile up to 12% in the high-pressure (HP) stage, and hydrothermal interactions during granite emplacement.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Geysson de Almeida Lages, Elton Luiz Dantas,