Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a) (2021)
- Authors:
- USP affiliated authors: TRINDADE, RICARDO IVAN FERREIRA DA - IAG ; JOVANE, LUIGI - IO
- Unidades: IAG; IO
- DOI: 10.1016/j.gloplacha.2021.103461
- Assunto: MERCÚRIO (ELEMENTO QUÍMICO)
- Language: Inglês
- Imprenta:
- Source:
- Título do periódico: Global and Planetary Change
- ISSN: 0921-8181
- Volume/Número/Paginação/Ano: v. 200, artigo 103461, 2021
- Este periódico é de assinatura
- Este artigo é de acesso aberto
- URL de acesso aberto
- Cor do Acesso Aberto: green
-
ABNT
PERCIVAL, L. M. E. et al. Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a). Global and Planetary Change, v. 200, 2021Tradução . . Disponível em: https://doi.org/10.1016/j.gloplacha.2021.103461. Acesso em: 19 abr. 2024. -
APA
Percival, L. M. E., Tedeschi, L. R., Creaser, R. A., Bottini, C., Erba, E., Giraud, F., et al. (2021). Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a). Global and Planetary Change, 200. doi:10.1016/j.gloplacha.2021.103461 -
NLM
Percival LME, Tedeschi LR, Creaser RA, Bottini C, Erba E, Giraud F, Svensen H, Savian J, Trindade RIF da, Coccioni R, Frontalini F, Jovane L, Mather TA, Jenkyns HC. Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a) [Internet]. Global and Planetary Change. 2021 ; 200[citado 2024 abr. 19 ] Available from: https://doi.org/10.1016/j.gloplacha.2021.103461 -
Vancouver
Percival LME, Tedeschi LR, Creaser RA, Bottini C, Erba E, Giraud F, Svensen H, Savian J, Trindade RIF da, Coccioni R, Frontalini F, Jovane L, Mather TA, Jenkyns HC. Determining the style and provenance of magmatic activity during the Early Aptian Oceanic Anoxic Event (OAE 1a) [Internet]. Global and Planetary Change. 2021 ; 200[citado 2024 abr. 19 ] Available from: https://doi.org/10.1016/j.gloplacha.2021.103461 - Mid-Cretaceous marine Os isotope evidence for heterogeneous cause of oceanic anoxic events
- High-resolution magneto-biostratigraphy of the early Eocene to early Oligocene from Indian Hole 711A and Italian Monte Cagnero section
- Middle Eocene to Early Oligocene climate: preliminary magnetobiostratigraphic from Monte Cagnero section, central Italy
- Middle Eocene Climatic Optimum (MECO) in the Monte Cagnero section, Central Italy
- Long-term Aptian marine osmium isotopic record of Ontong Java Nui activity
- Enhanced primary productivity and magnetotactic bacterial production in response to middle Eocene warming in the Neo-Tethys Ocean
- The Barremian-Aptian boundary in the Poggio le Guaine core (central Italy): evidence for magnetic polarity Chron M0r and oceanic anoxic event 1a
- Mixed Carbonate–Siliciclastic Sedimentation Along the Great Barrier Reef Upper Slope: A Challenge To the Reciprocal Sedimentation Model
- The Romanche fracture zone influences the segmentation of the equatorial margin of Brazil
- Magnetic methods and the timing of geological processes
Informações sobre o DOI: 10.1016/j.gloplacha.2021.103461 (Fonte: oaDOI API)
How to cite
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
