Diamond sources of the Juína region, Amazonian craton: textural and mineral chemical characteristics of Kimberley-type pyroclastic kimberlites (2024)
- Authors:
- USP affiliated authors: RUBERTI, EXCELSO - IGC ; AZZONE, ROGÉRIO GUITARRARI - IGC
- Unidade: IGC
- Subjects: DIAMANTE; KIMBERLITO
- Language: Inglês
- Conference titles: International Kimberlite Conference
-
ABNT
CABRAL NETO, Izaac et al. Diamond sources of the Juína region, Amazonian craton: textural and mineral chemical characteristics of Kimberley-type pyroclastic kimberlites. 2024, Anais.. [S.l.]: Instituto de Geociências, Universidade de São Paulo, 2024. Disponível em: https://repositorio.usp.br/directbitstream/cb92e01d-9efe-4189-804f-82c7c083a5a6/3255104.pdf. Acesso em: 28 dez. 2025. -
APA
Cabral Neto, I., Ruberti, E., Pearson, D. G., Luo, Y., Azzone, R. G., Silveira, F. V., & Almeida, V. V. (2024). Diamond sources of the Juína region, Amazonian craton: textural and mineral chemical characteristics of Kimberley-type pyroclastic kimberlites. In . Instituto de Geociências, Universidade de São Paulo. Recuperado de https://repositorio.usp.br/directbitstream/cb92e01d-9efe-4189-804f-82c7c083a5a6/3255104.pdf -
NLM
Cabral Neto I, Ruberti E, Pearson DG, Luo Y, Azzone RG, Silveira FV, Almeida VV. Diamond sources of the Juína region, Amazonian craton: textural and mineral chemical characteristics of Kimberley-type pyroclastic kimberlites [Internet]. 2024 ;[citado 2025 dez. 28 ] Available from: https://repositorio.usp.br/directbitstream/cb92e01d-9efe-4189-804f-82c7c083a5a6/3255104.pdf -
Vancouver
Cabral Neto I, Ruberti E, Pearson DG, Luo Y, Azzone RG, Silveira FV, Almeida VV. Diamond sources of the Juína region, Amazonian craton: textural and mineral chemical characteristics of Kimberley-type pyroclastic kimberlites [Internet]. 2024 ;[citado 2025 dez. 28 ] Available from: https://repositorio.usp.br/directbitstream/cb92e01d-9efe-4189-804f-82c7c083a5a6/3255104.pdf - Complexo alcalino máfico-ultramafico Ponte Nova (SP):: parte da província Serra do Mar ou uma província ígnea distinta?
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