Cargando…

Causes and consequences of asymmetric lateral plume flow during South Atlantic rifting

Volcanic rifted margins are typically associated with a thick magmatic layer of seaward dipping reflectors and anomalous regional uplift. This is conventionally interpreted as due to melting of an arriving mantle plume head at the onset of rifting. However, seaward dipping reflectors and uplift are...

Descripción completa

Detalles Bibliográficos
Autores principales: Morgan, Jason P., Taramón, Jorge M., Araujo, Mario, Hasenclever, Jörg, Perez-Gussinye, Marta
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2020
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7668071/
https://www.ncbi.nlm.nih.gov/pubmed/33106400
http://dx.doi.org/10.1073/pnas.2012246117