Interpretation of High-Resolution Remote Sensing Data for Plio-Pleistocene Tectonic Structures Studies in the Trindade Island Volcanic Building, South Atlantic Ocean, Brazil
Trindade Island (20°31′0’ S and 29°19′0 W) is a large alkaline volcanic edifice and is the only emerging part of the Vitória-Trindade ridge, 1140 km from the Brazilian offshore, whose summit is around 600 meters high. The lineament orientation pattern of Plio-Pleistocene dykes and fracture swarms id...
Guardado en:
| Autores principales: | , , , , , , , , |
|---|---|
| Formato: | Capítulo de libro |
| Lenguaje: | inglés |
| Publicado: |
IntechOpen
2024
|
| Materias: | |
| Acceso en línea: | https://www.intechopen.com/chapters/89253 |
| Etiquetas: |
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
| Sumario: | Trindade Island (20°31′0’ S and 29°19′0 W) is a large alkaline volcanic edifice and is the only emerging part of the Vitória-Trindade ridge, 1140 km from the Brazilian offshore, whose summit is around 600 meters high. The lineament orientation pattern of Plio-Pleistocene dykes and fracture swarms identified by high-resolution remote sensing allowed identifying the paleo-stresses that acted on Trindade Island. Our research suggests that Trindade Island suffered two distinct tectonic events between 3.6 Ma and 0.25 Ma: the first event is related to the island formation and shows a NW-SE (compressional) and NE-SW (extensional) stress orientation, while the second event shows different stress, namely ENE-WSW (compressional) and NNW-SSE (extensional). These events may also be associated with the opening of the South Atlantic Ocean, during movement and torsion of the South American Plate in the NE-SW direction, evidencing compression toward ENE or due to the influence of the Trindade mantle plume on the South American Plate which generated intraplate stress. |
|---|---|
| ISBN: | 978-1-83769-186-9 |
| DOI: | 10.5772/intechopen.113254 |