RT Journal Article
T1 New data (U–Pb, K–Ar) on the geochronology of thealkaline-carbonatitic association of Fuerteventura,Canary Islands, Spain
A1 Muñoz García, Mercedes
A1 Sagredo Ruiz, Juana
A1 Ignacio San José, Cristina de
A1 Fernández Suárez, Javier
A1 Jeffries, Teresa E.
AB Zircons from a nepheline-syenite of the Fuerteventura Basal Complex were dated by Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS). The age obtained from a total of 21 U–Th–Pb analyses is 25.4F0.3 Ma (2r) indicating a late Oligocene–early Miocene crystallization. This age is consistent with new K–Ar ages on nepheline-syenites and pyroxenites, and contradicts previously published 39Ar–40Ar (feldspar) ages that were interpreted to represent a late Cretaceous–early Paleocene, pyroxenitic–syenitic magmatic episode. These new geochronological data are consistent with both field observations and most of the previously published ages on alkaline silicate rocks and associated carbonatites of Fuerteventura. Therefore, they strongly support the existence of a single, late Oligocene–early Miocene event of alkaline–carbonatitic magmatism in the Basal Complex of Fuerteventura, taking place at approximately 25 Ma and comprising: alkaline-pyroxenites, melteigites-ijolites, nepheline-syenites and  carbonatites, as well as their volcanic equivalents and associated dykes. These new data provide an estimate for the length of time that it took the island to grow, thus eliminating one of the major problems in explaining its development by a hot-spot model.
PB Elsevier Science B.V., Amsterdam
SN 0024-4937
YR 2005
FD 2005
LK https://hdl.handle.net/20.500.14352/52394
UL https://hdl.handle.net/20.500.14352/52394
LA eng
DS Docta Complutense
RD 2 may 2024