Corrigendum to Unveiling geological complexity in the Serra Dourada Granite using self-organizing maps and hierarchical clustering: Insights for REE prospecting in the Goiás Tin Province, Brasília Belt, Central Brazil Journal of the Geological Survey of Brazil, 8 (1):51-63 (2025)
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Refers to: Unveiling geological complexity in the Serra Dourada Granite using self-organizing maps and hierarchical clustering: Insights for REE prospecting in the Goiás Tin Province, Brasília Belt, Central Brazil.
Journal of the Geological Survey of Brazil, Volume 8 (1), April 2025, pages 51-63.
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Following a request from an author/reader regarding the lack of proper attribution to his work in our article, we apologize for the unintentional error and have added the correct credit as follows:
1) Page 53 (caption of Figure 1): Figure 1: a) Location of the Tocantins Province in Central Brazil; b) Study area in the central portion of the Brasília Belt; c) Simplified Geological Map of the Goias Tin Province and the placement of the granites from the Tocantins and Paranã Sub-Provinces (modified from Costa Filho 2020).
2) Page 53 (last paragraph): This is similar to the ages of 571 ± 24 Ma (Teixeira 2002) and 546 ± 11 Ma (Costa-Filho 2020), both using the U-Pb method in monazite and to 530 Ma reported by Hasui and Almeida (1970), in biotite from the Serra da Mesa granite.
Guilherme Ferreira da Silva and co-authors.
Reference: Costa-Filho D.S. 2020. Caracterização mineralógica e proveniência de Monazita-(Ce), Xenotima-(Y) e Zircão de Placer na Província Estanífera de Goiás : estão estes minerais relacionados com o granito tipo-A Serra Dourada? Dissertation. Instituto de Geociências, Universidade de Brasília, Brasília, Distrito Federal, 48 p. http://repositorio.unb.br/handle/10482/39482
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