Please use this identifier to cite or link to this item: http://hdl.handle.net/2445/16889
Title: Primitive Cretaceous island-arc volcanic rocks in eastern Cuba: the Téneme Fromation
Author: Proenza Fernández, Joaquín Antonio
Díaz-Martínez, R.
Iriondo, A.
Marchesi, C.
Melgarejo i Draper, Joan-Carles
Gervilla, F.
Garrido, C. J.
Rodriguez-Vega, A.
Lozano-Santacruz, R.
Blanco-Moreno, J. A.
Keywords: Geoquímica
Roques volcàniques
Cuba
Geochemistry
Volcanic rocks
Cuba
Issue Date: 2006
Publisher: Universitat de Barcelona (UB). Institut de Ciències de la Terra Jaume Almera (ICTJA). Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDEA). Universitat Autonònoma de Barcelona (UAB). Consejo Superior de Investigaciones Científicas (CSIC)
Abstract: The Téneme Formation is located in the Mayarí-Cristal ophiolitic massif and represents one of the three Cretaceous volcanic Formations established in northeastern Cuba. Téneme volcanics are cut by small bodies of 89.70 ± 0.50 Ma quarz-diorite rocks (Río Grande intrusive), and are overthrusted by serpentinized ultramafics. Téneme volcanic rocks are mainly basalts, basaltic andesites, andesites, and minor dacites, and their geochemical signature varies between low-Ti island arc tholeiites (IAT) with boninitic affinity (TiO2 0.4 %; high field strength elements N-type MORB) and typical oceanic arc tholeiites (TiO2 = 0.5-0.8 %). Basaltic rocks exhibit low light REE/Yb ratios (La/Yb 5), typical of intraoceanic arcs and are comparable to Maimón Formation in Dominican Republic (IAT, pre Albian) and Puerto Rican lavas of volcanic phase I (island arc tholeiites, Aptian to Early Albian). The mantle wedge signature of the Téneme Formation indicates a highly depleted MORB-type mantle source, without any contribution of E-MORB or OIB components. Our results suggest that Téneme volcanism represents a primitive oceanic island arc environment. If the Late Cretaceous age (Turonian or early Coniacian) proposed for Téneme Formation is correct, our results indicate that the Cretaceous volcanic rocks of eastern Cuba and the Dominican Republic are not segments of a single arc system, and that in Late Cretaceous (Albian-Campanian) Caribbean island arc development is not represented only by calc-alkaline (CA) volcanic rocks as has been suggested in previous works.
Note: Reproducció del document publicat a http://www.geologica-acta.com/pdf/vol0401a06.pdf
It is part of: Geologica Acta, 2006, vol. 4, núm. 1-2, p. 103-121
Related resource: http://dx.doi.org/10.1344/105.000000360
URI: http://hdl.handle.net/2445/16889
ISSN: 1695-6133
Appears in Collections:Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)

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