é bacharel em Geologia (2012) pela Universidade de Brasília (UnB). Obteve mestrado na UnB em 2015, desenvolvendo um estudo sobre análise quantitativa da mineralogia de formações ferríferas por meio de dados espectrais. Em 2014, se tornou pesquisador em geociências do Serviço Geológico do Brasil (SGB), onde atuou no mapeamento geológico do estado de Rondônia por três anos. Atua desde 2019 como coordenador executivo do Centro de Geociências Aplicadas (CGA) do SGB, onde desenvolve pesquisas utilizando técnicas de inteligência artificial para criar soluções na área das geociências. Iniciou seu Ph.D. na Universidade de Campinas (Unicamp), em 2019, com o objetivo de investigar a aplicação de métodos de aprendizado de máquina na exploração de depósitos minerais do tipo IOCG. BIOGRAPHY Elias M. G. Prado has a bachelor's degree in Geology (2012) from the University of Brasília (UnB). He obtained a master's degree from UnB in 2015, developing a study on quantitative analysis of the mineralogy of iron formations through spectral data. In 2014, he became a researcher in geosciences at the Geological Survey of Brazil (SGB), where he worked on the geological mapping of the state of Rondônia for three years. He has served since 2019 as executive coordinator of the SGB's Center for Applied Geosciences (CGA), where he develops research using artificial intelligence techniques to create solutions in the geosciences. He started a Ph.D. at the University of Campinas (Unicamp) in 2019, aiming to investigate the application of machine learning methods in the exploration of IOCG-type mineral deposits. AGRADECIMENTO To my father, Edson, in loving memory. To my mother, Germana, and sister, Cássia, my sincere thanks for the caring, example, and full support. To my wife Flávia and son Caio, thanks for the companionship, encouragement and all the support. I thank Prof. Dr. Carlos Roberto de Souza Filho of the University of Campinas (UNICAMP) for his dedication and guidance during this learning period. To the Prof. E. John Carranza of the University of the Free State (Bloemfontein, South Africa) for the great collaboration in this work. I thank the Geological Survey of Brazil (SGB) for the release for training through internal selection process. I direct this acknowledgment to the head of the Applied Geosciences Center (CGA) of the SGB, Noevaldo Araujo Teixeira, who supports my work so many times To the various geologists and colleagues in Brazil who participate directly or indirectly in the research. To João Motta, Leandro, Rodrigo, Cimara, and Christian for all the support and knowledge exchange.