F
Filipe Brandão
Publications - 5
Citations - 80
Filipe Brandão is an academic researcher. The author has contributed to research in topics: Clathrate hydrate & Lava. The author has an hindex of 3, co-authored 5 publications receiving 67 citations.
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The insular shelves of the Faial-Pico Ridge (Azores archipelago): A morphological record of its evolution
Rui Quartau,Rui Quartau,José Firmino Aguilar Madeira,Neil C. Mitchell,Fernando Tempera,Pedro Silva,Pedro Silva,Filipe Brandão +7 more
TL;DR: In this paper, multibeam bathymetry, high-resolution seismic reflection profiles, and sediment samples are used to characterize the morphology of the insular shelves adjacent to Pico Island.
Journal ArticleDOI
Reply to comment by Marques et al. on “The insular shelves of the Faial‐Pico Ridge (Azores archipelago): A morphological record of its evolution”
Rui Quartau,Rui Quartau,José Madeira,Neil C. Mitchell,Fernando Tempera,Pedro Silva,Filipe Brandão +6 more
TL;DR: In this article, multibeam bathymetry, high-resolution seismic reflection profiles, and sediment samples are used to characterize the morphology of the insular shelves adjacent to Pico Island.
Journal ArticleDOI
Determination of Priority Study Areas for Coupling CO2 Storage and CH4 Gas Hydrates Recovery in the Portuguese Offshore Area
TL;DR: In this article, a determination of the areas with conditions for the formation of biogenic gas hydrates in Portugal's mainland geological continental margin and assesses their overlap with CO2 hydrate stability zones defined in previous studies is presented.
Acoustic evidences of along-slope processes associated with mass movement deposits on the Madeira Island lower slope (Eastern Central Atlantic).
C. Roque,Pedro Madureira,Francisco Javier Hernandéz-Molina,A. Santos de Campos,Rui Quartau,Gabriela Carrara,Filipe Brandão,Juan Tomás Vázquez,L. Somoza +8 more
TL;DR: A plastered contourite drift (Madeira drift) developed on this lower slope, being composed of seismic units D1, D2 and D3 as discussed by the authors, and the most probable water mass responsible for its deposition is the Antarctica Bottom Water (AABW).