Use este identificador para citar ou linkar para este item:
http://www.repositorio.ufop.br/jspui/handle/123456789/11215
Título: | U-Pb geochronology of Paraná volcanics combined with trace element geochemistry of the zircon crystals and zircon Hf isotope data. |
Autor(es): | Hartmann, Leo Afraneo Baggio, Sergio Benjamin Brückmann, Matheus Philipe Knijnik, Daniel Barbosa Lana, Cristiano de Carvalho Massonne, Hans-Joachim Opitz, Joachim Pinto, Viter Magalhães Sato, Kei Tassinari, Colombo Celso Gaeta Arena, Karine da Rosa |
Palavras-chave: | Paraná volcanic province U-Pb age εHf Trace elements |
Data do documento: | 2019 |
Referência: | HARTMANN, L. A. et al. U-Pb geochronology of Paraná volcanics combined with trace element geochemistry of the zircon crystals and zircon Hf isotope data. Journal of South American Earth Sciences, v. 1, p. 1-21, 2018. Disponível em: <https://www.sciencedirect.com/science/article/pii/S0895981118300622>. Acesso em: 08 fev. 2019. |
Resumo: | The Paraná volcanic province is a window into mantle and crustal processes in the Cretaceous. The variability and complexity of this province can be determined through the study of minerals. An integrated study of zircon from Paraná lavas (one high-Ti basalt, one low-Ti andesite, one high-Ti rhyodacite and one high-Ti andesite sill) was achieved using backscattered electron imaging, sensitive high resolution ion microprobe (SHRIMP-IIe) for U-Pb geochronology, and laser ablation inductively coupled mass spectrometer (LA-ICPMS) to determine the Lu- Hf isotopes and the trace-element compositions. U-Pb-Hf and trace-element data indicate that zircon crystallized from the magma at approximately 134 Ma. This South American large igneous province originated from the mantle and was contaminated by crust either in the mantle or during ascent and crystallization of magma. Contaminant continental crust had Precambrian age. Trace elements point to a new compositional field for zircon, different from other types of provinces. Examination of volcanic zircon improves our understanding of age and contamination of the Paraná volcanics. |
URI: | http://www.repositorio.ufop.br/handle/123456789/11215 |
Link para o artigo: | https://www.sciencedirect.com/science/article/pii/S0895981118300622 |
DOI: | https://doi.org/10.1016/j.jsames.2018.11.026 |
ISSN: | 0895-9811 |
Aparece nas coleções: | DEGEO - Artigos publicados em periódicos |
Arquivos associados a este item:
Arquivo | Descrição | Tamanho | Formato | |
---|---|---|---|---|
ARTIGO_U-PbGeochronologyParaná.pdf Restricted Access | 2,1 MB | Adobe PDF | Visualizar/Abrir |
Os itens no repositório estão protegidos por copyright, com todos os direitos reservados, salvo quando é indicado o contrário.