Primitive Cretaceous island-arc volcanic rocks in eastern Cuba: The Téneme Formation


Por: Proenza J.A., Díaz-Martínez R., Iriondo A., Marchesi C., Melgarejo J.C., Gervilla F., Garrido C.J., Rodríguez-Vega A., Lozano-Santacruz R., Blanco-Moreno J.A.

Publicada: 1 ene 2006
Resumen:
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 Uneme 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. © UB-ICTJA.

Filiaciones:
Departament de Cristal-Iografia, Mineralogia i Dipòsits Minerals, Facultat de Geologia, Universitat de Barcelona, Martí i Franquès s/n, 08028 Barcelona, Spain
Departamento de Geología, Instituto Superior Minero Metalúrgico de Moa, Las Coloradas s/n, 83320 Moa, Holguín, Cuba
Centro de Geosciencias, Universidad Nacional Autónoma de México, Campus Juriquilla, 76230 Juriquilla, Querétaro, Mexico
Department of Geological Sciences, University of Colorado at Boulder, Boulder, CO 80309, United States
Departamento de Mineralogía y Petrología, Facultad de Ciencias, Universidad de Granada, Avenida Fuentenueva s/n, 18002 Granada, Spain
Instituto de Geología, Universidad Nacional Autónoma de México, Coyoacán 04510 Mexico D.F., Mexico
ISSN: 16956133
Editorial
UNIV BARCELONA, INST CIENCIES TERRA JAUME ALMERA-CSIC, LLUIS SOLE I SABARIS S-N, BARCELONA, E-08028, SPAIN, España
Tipo de documento: Article
Volumen: 4 Número: 1-2
Páginas: 103-121

MÉTRICAS