Paleomagnetism of IODP Site U1380: implications for the forearc deformation in the Costa Rican erosive convergent margin (2018)
- Autores:
- Autor USP: JOVANE, LUIGI - IO
- Unidade: IO
- DOI: 10.1038/s41598-018-29243-7
- Assunto: PALEOMAGNETISMO
- Idioma: Inglês
- Imprenta:
- Fonte:
- Título do periódico: Scientific Reports
- ISSN: 2045-2322
- Volume/Número/Paginação/Ano: v. 8, Artigo 11430, 2018
- Este periódico é de acesso aberto
- Este artigo é de acesso aberto
- URL de acesso aberto
- Cor do Acesso Aberto: gold
- Licença: cc-by
-
ABNT
LI, Yong-Xiang et al. Paleomagnetism of IODP Site U1380: implications for the forearc deformation in the Costa Rican erosive convergent margin. Scientific Reports, v. 8, 2018Tradução . . Disponível em: https://doi.org/10.1038/s41598-018-29243-7. Acesso em: 19 abr. 2024. -
APA
Li, Y. -X., Zhao, X., Xie, S., Jovane, L., & Petronotis, K. (2018). Paleomagnetism of IODP Site U1380: implications for the forearc deformation in the Costa Rican erosive convergent margin. Scientific Reports, 8. doi:10.1038/s41598-018-29243-7 -
NLM
Li Y-X, Zhao X, Xie S, Jovane L, Petronotis K. Paleomagnetism of IODP Site U1380: implications for the forearc deformation in the Costa Rican erosive convergent margin [Internet]. Scientific Reports. 2018 ; 8[citado 2024 abr. 19 ] Available from: https://doi.org/10.1038/s41598-018-29243-7 -
Vancouver
Li Y-X, Zhao X, Xie S, Jovane L, Petronotis K. Paleomagnetism of IODP Site U1380: implications for the forearc deformation in the Costa Rican erosive convergent margin [Internet]. Scientific Reports. 2018 ; 8[citado 2024 abr. 19 ] Available from: https://doi.org/10.1038/s41598-018-29243-7 - Mixed Carbonate–Siliciclastic Sedimentation Along the Great Barrier Reef Upper Slope: A Challenge To the Reciprocal Sedimentation Model
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Informações sobre o DOI: 10.1038/s41598-018-29243-7 (Fonte: oaDOI API)
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