Source: Journal of Geology. Unidade: IGC
Assunto: GEOCRONOLOGIA
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CARDONA, Agustin et al. U-Pb Zircon Geochronology and Nd Isotopic Signatures of the Pre-Mesozoic Metamorphic Basement of the Eastern Peruvian Andes: Growth and Provenance of a Late Neoproterozoic to Carboniferous Accretionary Orogen on the Northwest Margin of Gondwana. Journal of Geology, v. 117, n. 3, 2009Tradução . . Disponível em: https://doi.org/10.1086/597472. Acesso em: 14 nov. 2024.APA
Cardona, A., Cordani, U. G., Ruiz, J., Valencia, V. A., Armstrong, R., Chew, D., et al. (2009). U-Pb Zircon Geochronology and Nd Isotopic Signatures of the Pre-Mesozoic Metamorphic Basement of the Eastern Peruvian Andes: Growth and Provenance of a Late Neoproterozoic to Carboniferous Accretionary Orogen on the Northwest Margin of Gondwana. Journal of Geology, 117( 3). doi:10.1086/597472NLM
Cardona A, Cordani UG, Ruiz J, Valencia VA, Armstrong R, Chew D, Nutman A, Sanchez AW. U-Pb Zircon Geochronology and Nd Isotopic Signatures of the Pre-Mesozoic Metamorphic Basement of the Eastern Peruvian Andes: Growth and Provenance of a Late Neoproterozoic to Carboniferous Accretionary Orogen on the Northwest Margin of Gondwana [Internet]. Journal of Geology. 2009 ; 117( 3):[citado 2024 nov. 14 ] Available from: https://doi.org/10.1086/597472Vancouver
Cardona A, Cordani UG, Ruiz J, Valencia VA, Armstrong R, Chew D, Nutman A, Sanchez AW. U-Pb Zircon Geochronology and Nd Isotopic Signatures of the Pre-Mesozoic Metamorphic Basement of the Eastern Peruvian Andes: Growth and Provenance of a Late Neoproterozoic to Carboniferous Accretionary Orogen on the Northwest Margin of Gondwana [Internet]. Journal of Geology. 2009 ; 117( 3):[citado 2024 nov. 14 ] Available from: https://doi.org/10.1086/597472