Articles | Volume 6, issue 1
Solid Earth, 6, 227–241, 2015
https://doi.org/10.5194/se-6-227-2015
Solid Earth, 6, 227–241, 2015
https://doi.org/10.5194/se-6-227-2015

Research article 19 Feb 2015

Research article | 19 Feb 2015

Volcanological aspects of the northwest region of Paraná continental flood basalts (Brazil)

F. Braz Machado et al.

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement
Download
Short summary
This study describes for the first time morphological aspects of lava flows and structural characteristics caused by lava-sediment interaction in the northwestern Paraná continental flood basalts in the southeast of the South American Plate (Brazil). Early Cretaceous (134 to 132Ma) tholeiitic rocks were emplaced on a large intracratonic Paleozoic sedimentary basin (Paraná Basin), mainly covering dry eolian sandstones (Botucatu Formation).