Relocation of hypocenters of the induced activity in Bebedouro, Paraná Basin, Brazil (2010)
- Authors:
- USP affiliated authors: ASSUMPCAO, MARCELO SOUSA DE - IAG ; BARBOSA, JOSE ROBERTO - IAG
- Unidade: IAG
- Subjects: SISMOLOGIA; BACIA DO PARANÁ
- Language: Inglês
- Imprenta:
- Publisher: American Geophysical Union
- Publisher place: Washington
- Date published: 2010
- Source:
- Conference titles: 2010 Meeting of the Americas
-
ABNT
DICELIS, G e ASSUMPÇÃO, Marcelo Souza de e BARBOSA, José Roberto. Relocation of hypocenters of the induced activity in Bebedouro, Paraná Basin, Brazil. 2010, Anais.. Washington: American Geophysical Union, 2010. . Acesso em: 12 mar. 2026. -
APA
Dicelis, G., Assumpção, M. S. de, & Barbosa, J. R. (2010). Relocation of hypocenters of the induced activity in Bebedouro, Paraná Basin, Brazil. In Eos Transactions AGU, v.91, n.26, Meeting of the Americas Supplement, abstract S41A-05, 2010. Washington: American Geophysical Union. -
NLM
Dicelis G, Assumpção MS de, Barbosa JR. Relocation of hypocenters of the induced activity in Bebedouro, Paraná Basin, Brazil. Eos Transactions AGU, v.91, n.26, Meeting of the Americas Supplement, abstract S41A-05, 2010. 2010 ;[citado 2026 mar. 12 ] -
Vancouver
Dicelis G, Assumpção MS de, Barbosa JR. Relocation of hypocenters of the induced activity in Bebedouro, Paraná Basin, Brazil. Eos Transactions AGU, v.91, n.26, Meeting of the Americas Supplement, abstract S41A-05, 2010. 2010 ;[citado 2026 mar. 12 ] - Estudos preliminares da sismicidade registrada em Montes Claros, Minas Gerais
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- O sismo do Pantanal de 2009: caracterização e implicações tectônicas
- Determination of basement depth and basalt thickness in the Paraná basin with high-frequency receiver function
- Estudo da sismicidade induzida no reservatório de Miranda, MG
- The 2012 Montes Claros earthquake sequence in the São Francisco craton: another evidence of inverse faulting and compressional stresses in Eastern Brazil
- An improved velocity model for regional epicentre determination in Brazil
- Atividade sísmica na Bacia do Paraná induzida pela perfuração de poçços tubulares profundos
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