Source: Ofioliti. Unidade: IGC
Subjects: GEOQUÍMICA, PETROLOGIA, ROCHAS MÁFICAS, ROCHAS ULTRAMÁFICAS, ORDOVICIANO
ABNT
PEDRO, Jorge et al. Geochemistry and U-PB zircon age of the internal Ossa-Morena zone ophiolite sequences: a remnant of Rheic Ocean in SW Iberia. Ofioliti, v. 35, n. 2, p. 117-130, 2010Tradução . . Disponível em: https://doi.org/10.4454/ofioliti.v35i2.390. Acesso em: 17 out. 2024.APA
Pedro, J., Araujo, A., Fonseca, P., Tassinari, C. C. G., & Ribeiro, A. (2010). Geochemistry and U-PB zircon age of the internal Ossa-Morena zone ophiolite sequences: a remnant of Rheic Ocean in SW Iberia. Ofioliti, 35( 2), 117-130. doi:10.4454/ofioliti.v35i2.390NLM
Pedro J, Araujo A, Fonseca P, Tassinari CCG, Ribeiro A. Geochemistry and U-PB zircon age of the internal Ossa-Morena zone ophiolite sequences: a remnant of Rheic Ocean in SW Iberia [Internet]. Ofioliti. 2010 ; 35( 2): 117-130.[citado 2024 out. 17 ] Available from: https://doi.org/10.4454/ofioliti.v35i2.390Vancouver
Pedro J, Araujo A, Fonseca P, Tassinari CCG, Ribeiro A. Geochemistry and U-PB zircon age of the internal Ossa-Morena zone ophiolite sequences: a remnant of Rheic Ocean in SW Iberia [Internet]. Ofioliti. 2010 ; 35( 2): 117-130.[citado 2024 out. 17 ] Available from: https://doi.org/10.4454/ofioliti.v35i2.390