Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.12136/573
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Title: Volcano-stratigraphic and structural evolution of Brava Island (Cape Verde) based on 40Ar/39Ar, U-Th and field constraints
Authors: Madeira, José ‎
Mata, João
Mourão, Cyntia Coquelet Pinto
Silveira, António Pedro Valério Brum da
Martins, Sofia Maria Marques
Ramalho, Ricardo dos Santos
Hoffmann, Dirk
Keywords: Cape Verde;Brava Island;40Ar/39Ar dating;Volcano-stratigraphy;Uplift
Issue Date: Oct-2010
Publisher: Elsevier
Citation: Journal of Volcanology and Geothermal Research, 2010, 196 (3-4), 219-235
Abstract: Three volcano-stratigraphic units were identified at Brava Island in the Cape Verde Archipelago on the basis of field relationships, geologic mapping and 40Ar/39Ar and U–Th ages. The Lower Unit comprises a 2-to-3 Ma-old submarine volcanic sequence that represents the seamount stage. It is composed of nephelinitic/ankaramitic hyaloclastites and pillow lavas, which are cut by abundant co-genetic dikes. Plutonic rocks of an alkaline–carbonatite complex, which intruded the submarine sequence 1.8 to 1.3 Ma ago, constitute the Middle Unit. A major erosional surface developed between 1.3 and ~ 0.25 Ma. The post-erosional volcanism recorded in the Upper Unit started 0.25 Ma ago and is dominated by phonolitic magmatism. This phase is characterised by explosive phreato-magmatic and magmatic activity that produced block and ash flow, surge, and pyroclastic fall deposits and numerous phreato-magmatic craters. Effusive events are represented by lava domes and coulées. One peculiarity of Brava is the occurrence of carbonatites in both the plutonic complex and the post-erosional phase as extrusive volcanics. The intrusive carbonatites are younger than those occurring on Fogo, Santiago and Maio islands. Young (Upper Pleistocene to Holocene) extrusive carbonatites occurring in the late stages of volcanism are unknown in other Cape Verde islands. The occurrence of pillow lavas and hyaloclastites above the present sea level (up to 400 m) and raised Upper Pleistocene beaches indicates continuous uplift of Brava since the seamount stage. By dating raised marine markers, uplift rates were estimated at between 0.2 and 0.4 mm/a. The evolution of Brava was controlled by faults with directions similar to those described for Fogo, suggesting a common stress field.
URI: http://hdl.handle.net/20.500.12136/573
ISSN: 0377-0273
DOI: 10.1016/j.jvolgeores.2010.07.010
Editor version: https://doi.org/10.1016/j.jvolgeores.2010.07.010
Type: Article
Appears in Collections:Geocronología y Geología



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