Search

This study focuses on the tectonic control of post-rift Eocene alkaline intrusions that outcrop in the Atalaia Peninsula, SE Brazil, on the onshore limit of both the Campos and Santos basins, the most prolific Brazilian oil basins. To investigate these tectonic-magmatic processes, high-resolution unmanned aerial vehicle (UAV) images, structural field data, and geochronological analyses were performed. This study characterized several alkaline lithotypes (syenites, N–S and NW–SE trachytes, NW–SE lamprophyres, and E–W phonolites dikes), cutting a N–S oriented Paleoproterozoic orthogneiss basement and NE–SW tholeiitic dikes. A new Ar–Ar age of 53.82 ± 0.7 Ma was obtained on phlogopite from one lamprophyre dike. Geometric and dynamic analysis indicate that these alkaline intrusions are synchronous and their emplacements can be explained by a sub-horizontal NNE–SSW intraplate extension linked to a sub-vertical σ 1. Magma rising occurred by forceful injection through transcrustal sets of discontinuities that reached the mantle. Strike to oblique-slip and late normal faults support an anticlockwise rotational extension direction after emplacement. These alkaline tectonic-magmatic dynamics may have caused an isostatic response, influencing the evolution of the abutting offshore basins while triggering a large influx of sediments during the Paleocene-Eocene. • Structural analysis using high-resolution UAV images focused on alkaline dikes. • New Ar–Ar geochronological data indicate 53.82 ± 0.7 Ma for a lamprophyre dike. • Coeval alkaline magmas from mantle sources. • Reactivation of pre-existing discontinuities as magma conduits. • Magma rise may be related to the lithospheric flexure and sediment influx offshore. [ABSTRACT FROM AUTHOR]