Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
9525900 | Journal of Geodynamics | 2005 | 12 Pages |
Abstract
Domal uplift, a giant tholeiitic mafic dyke swarm, anorogenic bimodal volcanism and plutonism and extensive intracontinental rift sedimentary sequences are recorded at the Late Paleoproterozoic of the Central and Southeastern Brazil. Mantle plume events at 1.77Â Ga and around 1.72Â Ga are thought as an unifying concept for these geological features.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Alexandre de Oliveira Chaves, José Marques Correia Neves,