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...
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| 發表在: | Anais da Academia Brasileira de Ciências |
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| Principais autores: | , , , |
| 格式: | Artigo |
| 語言: | Inglês |
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Academia Brasileira de Ciências
2008
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| 主題: | |
| 在線閱讀: | https://www.redalyc.org/articulo.oa?id=32713458014 |
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