Geochemistry and petrogenesis of post-collisional ultrapotassic syenites and granites from southernmost Brazil: the Piquiri Syenite Massif
The Piquiri Syenite Massif, southernmost Brazil, is part of the post-collisional magmatism related to the Neoproterozoic Brasiliano-Pan-African Orogenic Cycle. The massif is about 12 km in diameter and is composed of syenites, granites, monzonitic rocks and lamprophyres. Diopside-phlogopite, diopsid...
Sábháilte in:
| Foilsithe in: | Anais da Academia Brasileira de Ciências |
|---|---|
| Príomhchruthaitheoirí: | , , , |
| Formáid: | Artigo |
| Teanga: | Inglês |
| Foilsithe / Cruthaithe: |
Academia Brasileira de Ciências
2008
|
| Ábhair: | |
| Rochtain ar líne: | https://www.redalyc.org/articulo.oa?id=32713458014 |
| Clibeanna: |
Níl clibeanna ann, Bí ar an gcéad duine le clib a chur leis an taifead seo!
|