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

Authors

  • J.A. PROENZA FERNÁNDEZ Facultat de Geologia, Universitat de Barcelona
  • R. DÍAZ-MARTÍNEZ Instituto Superior Minero Metalúrgico de Moa
  • A. IRIONDO Centro de Geociencias, Universidad Nacional Autónoma de México and Department of Geological Sciences, University of Colorado at Boulder
  • C. MARCHESI Facultad de Ciencias, Universidad de Granada
  • Joan-Carles Melgarejo i Draper Facultat de Geologia, Universitat de Barcelona
  • F. GERVILLA LINARES Facultad de Ciencias, Universidad de Granada
  • C. J. GARRIDO MARÍN Facultad de Ciencias, Universidad de Granada
  • A. RODRÍGUEZ VEGA Instituto Superior Minero Metalúrgico de Moa
  • J. A. BLANCO-MORENO Instituto Superior Minero Metalúrgico de Moa
  • R. LOZANO-SANTACRUZ nstituto de Geología, Universidad Nacional Autónoma de México

DOI:

https://doi.org/10.1344/105.000000360

Keywords:

Geochemistry, Volcanic rocks, Primitive-island arc, Téneme Formation, Cuba

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.

Author Biographies

J.A. PROENZA FERNÁNDEZ, Facultat de Geologia, Universitat de Barcelona

Departament de Cristal·lografia, Mineralogia i Dipòsits Minerals

R. DÍAZ-MARTÍNEZ, Instituto Superior Minero Metalúrgico de Moa

Departamento de Geologí

C. MARCHESI, Facultad de Ciencias, Universidad de Granada

Departamento de Mineralogía y Petrología

Joan-Carles Melgarejo i Draper, Facultat de Geologia, Universitat de Barcelona

Departament de Cristal·lografia, Mineralogia i Dipòsits Minerals

F. GERVILLA LINARES, Facultad de Ciencias, Universidad de Granada

Departamento de Mineralogía y Petrología

C. J. GARRIDO MARÍN, Facultad de Ciencias, Universidad de Granada

Departamento de Mineralogía y Petrología

A. RODRÍGUEZ VEGA, Instituto Superior Minero Metalúrgico de Moa

Departamento de Geología

J. A. BLANCO-MORENO, Instituto Superior Minero Metalúrgico de Moa

Departamento de Geología

References

Adamovich, A.F., Chejovich, V.D., Trubino, D.Y., Shirikov, V.M., Pavlov, A.N., 1963. Estructura geológica y los minerales útiles de los macizos montañosos de Sierra de Nipe y Sierra Cristal, provincia de Oriente. Oficina Nacional de Recursos Minerales de Cuba, (unpublished).

Barnes, S.J., Roeder, P.L., 2001. The range of spinel compositions in terrestrial mafic and ultramafic rocks. Journal of Petrology, 42, 2279-2302.

Beccaluva, L., Macciotta, G., Piccardo, G.B., Zeda, O., 1989. Clinopyroxene compositions of ophiolites basalts as petrogenetic indicator. Chemical Geology, 77, 165-182.

Bortolotti, V., Marroni, M., Pandolfi, L., Principi, G., Saccani, E., 2002. Interaction between Mid-ocean ridge and subduction magmatism in Albanian Ophiolites. The Journal of Geology, 100, 561-576.

Blein, O., Guillot, S., Lapierre, H., Mercier de Lépinay, B., Lardeaux, J.M., Millan-Trujillo, G., Campos, M., Garcia, A., 2003. Geochemistry of the Mabujina Complex, Central Cuba: implications on the Cuban Cretaceous arc rocks. The Journal of Geology, 111, 89-101.

Cebula, G.T., Kunk, M.J., Mehnert, H.H., Naeser, C.W., Obradovich, J.D., Sutter, J.F., 1986. The Fish Canyon Tuff: A potential standard for the 40Ar/39Ar and fission track dating methods. Terra Cognita, 6, 2, p. 140.

Cobiella-Reguera, J.L., 2005. Emplacement of Cuban ophiolites. Geological Acta, 3, 273-294.

Defant, M.J., Drummond, M.S., 1993. Mount St. Helens: potential example of the partial melting of the subducted lithosphere in a volcanic arc. Geology, 21, 547-550.

Díaz de Villalvilla, L., 1997. Caracterización geológica de las formaciones volcano-sedimentarias en Cuba Central, provincias Cienfuegos, Villa Clara, Sancti Spiritus. In: Furrazola, G.F., Nuñez-Cambra, K.E. (eds.). Estudios sobre Geología de Cuba. Ciudad de la Habana, Cuba, Instituto de Geología y Paleontología, 325-344.

Díaz de Villalvilla, L., Pérez, M., Sukar, K., Marí, T., Méndez, I., Rodríguez, R., Piñero, R., Quintana, M.E., Aguirre, G., Echevarría, B., Milia, I., 1994. Consideraciones geoquímicas acerca de los arcos volcánicos de Cuba. Segundo Congreso Cubano de Geología y Minería. Libro de Programas y Resúmenes, Santiago de Cuba, p. 173.

Donnelly, T.W., Beets, D.J., Carr, M.J., Jackson, T., Kalver, G., Lewis, J., Maury, R., Schellekens, H., Smith, A., Wadge, G., Westercamp, D., 1990. History and tectonic setting of Caribbean magmatism. In: Dengo, G., Case, J.E. (eds.). The Caribbean. Decade of North American Geology, Boulder, Colorado, Geological Society of America, Volume H, 339-374.

Donnelly, T.W., Rogers, J.J.W., 1980. Igneous series in island arc: the northern Caribbean compared worldwide island arc assemblages. Bulletin of Volcanology, 43, 347-382.

Gyarmati, P., Leyé O’Conor, J., 1990. Informe final sobre los trabajos de levantamiento geológico en escala 1:50 000 y búsqueda acompañante en el polígono CAME V, Guantánamo. Oficina Nacional de Recursos Minerales, Cuba. Gyarmati, P., Méndez, I., Lay, M., 1997. Caracterización de las rocas del arco de islas Cretácico en la Zona EstructuroFacial Nipe-Cristal-Baracoa. In: Furrazola, G.F., NuñezCambra, K.E (eds.). Estudios sobre Geología de Cuba. Ciudad de la Habana, Cuba, Instituto de Geología y Paleontología, 357-364.

Hawkesworth, C.J., Gallagher, K., Hergt, J.M., McDermott, F., 1993a. Mantle and slab contributions in arc magmas. Annual Reviews of Earth and Planetary Sciences, 21, 175-204.

Hawkesworth, C.J., Gallagher, K., Hergt, J.M., McDermott, F., 1993b. Trace elements fractionation processes in the generation of island arc basalts. Philosophical Transactions of the Royal Society of London, series A 342, 179-191.

Hawkins, J.W., Allan, J.F., 1994. Petrogenetic evolution of the Lau Basin sites 834 trough 839. Proceedings Ocean Drilling Program Scientific Results, 135, 427-470.

Iturralde-Vinent, M., 1976. Estratigrafía de la zona CalabazasAchotal, Mayarí Arriba, Oriente. La Minería en Cuba, 5, 9-23.

Iturralde-Vinent, M., 1994. Cuban Geology: A new plate tectonic synthesis. Journal of Petroleum Geology, 17, 39-70.

Iturralde-Vinent, M., 1996a. Geología de las ofiolitas de Cuba. In: Iturralde-Vinent, M. (ed.). Ofiolitas y arcos volcánicos de Cuba. Miami, USA, IGCP Project 364, 83-120.

Iturralde-Vinent, M., 1996b. Cuba: el arco de islas volcánicas del Cretácico. In: Iturralde-Vinent, M. (ed.). Ofiolitas y arcos volcánicos de Cuba. Miami, USA, IGCP Project 364, 179-189.

Iturralde-Vinent, M., 1996c. Evidencias de un arco primitivo (Cretácico Inferior) en Cuba. In: Iturralde-Vinent, M. (ed.). Ofiolitas y arcos volcánicos de Cuba. Miami, USA, IGCP Project 364, 227-230.

Iturralde-Vinent, M.A., 2003. The relationship between the ophiolites, the metamorphic terrains, the Cretaceous volcanic arcs and the Paleocene-Eocene volcanic arc. Field guide to a geological excursion to Eastern Cuba. V Cuban Geological and Mining Congress. IGCP Project 433 Caribben Plate Tectonics. Cuban Geological Society, 16 pp.

Iturralde-Vinent, M., Díaz-Otero, C., Rodríguez-Vega, A., DíazMartínez, R., 2006. Tectonic implications of paleontologic dating of Cretaceous-Danian sections of Eastern Cuba. Geologica Acta, 4, 89-102.

Jolly, W.T., Lidiak, E.G., Dickin, A.P., Wu, T.W., 2001. Secular geochemistry of central Puerto Rican island arc lavas: constraints on Mesozoic tectonism in the Eastern Greater Antilles. Journal of Petrology, 42, 2197-2214.

Jolly, W.T., Lidiak, E.G., Dickin, A.P., Wu, T.W., 2002. Recycling in the Puerto Rican mantle wedge, Greater Antilles island arc. The Island Arc, 11, 10-24.

Kerr, A.C., Iturralde-Vinent, M., Saunders, A.D., Babbs, T.L., Tarney, J., 1999. A new plate tectonic model of the Caribbean: Implications from a geochemical reconnaissance of Cuban Mesozoic volcanic rocks. Geological Society of America Bulletin, 111, 1581-1599.

Knipper, A.L., Cabrera, R., 1974. Téctonica y geología histórica de la zona de articulación entre el mio- y eugeosinclinal y del cinturón hiperbasítico de Cuba. Academia de Ciencias de Cuba, Instituto de Geología, Contribución a la geología de Cuba, 15-77.

Kunk, M. J., Sutter, J. F., Naeser, C. W., 1985. High-precision 40Ar/39Ar Ages of Sanidine, Biotite, Hornblende, and Plagioclase from the Fish Canyon Tuff, San Juan Volcanic Field, South-central Colorado. Geological Society of America Abstracts with Programs, 17, p. 636.

Kunk, M. J., Winick, J. A., Stanley, J.O., 2001. 40Ar/39Ar agespectrum and laser fusion data for volcanic rocks in west central Colorado. U.S. Geological Survey, Open-File Report 01-472, 94,pp.

Lebron, M.C., Perfit, M.R., 1993. Stratigraphic and petrochemical data support subduction polarity reversal of the Cretaceous Caribbean Island Arc. The Journal of Geology, 101, 389-396.

Lebron, M.C., Perfit, M.R., 1994. Chemistry and tectonic significance of Cretaceous island-arc rocks, Cordillera Oriental, Dominican Republic. Tectonophysics, 229, 69-100.

Leterrier, J., Maury, R.C., Thonon, P., Girard, D., Marchal, M., 1982. Clinopyroxene composition as a method of identification of the magmatic affinities of paleo-volcanic series. Earth Planetary Science Letters, 59, 139-154.

Lewis, J.F., Astacio, V.A., Espaillat, J., Jimenez, J., 2000. The occurrence of volcanogenic massive sulphide deposits in the Maimón Formation, Dominican Republic: The Cerro de Maimón, Loma Pesada and Loma Barbuito deposits. In: Sherlock, R. Barsch, R. Logan, A. (eds.). VMS deposits of Latin America. Geological Society of Canada Special Publication, 223-249.

Lewis, J.F., Escuder-Viruete, J., Hernaiz-Huerta, P.P., Gutiérrez, G., Draper, G., Pérez-Estaún, A., 2002. Subdivisión geoquímica del arco de Isla Circum-Caribeño, Cordillera Central Dominicana: Implicaciones para la formación, acreción y crecimiento cortical en un ambiente intraoceánico. Acta Geologica Hispanica, 37, 81-122.

Lewis, J.F., Perfit, M., Horan, S., Diaz de Villalvilla, L., 1995. Geochemistry and petrotectonic significance of early island arc bimodal volcanism in the Greater Antilles arc. Geological Society of America, Abstracts with Programs, New Orleans, Louisiana A-227.

Lidiak, E.G., Jolly, W.T., 1996. Circum-Caribbean granitoids: characteristics and origin. International Geology Review, 38, 1098-1133.

Lidiak, E.G., Jolly, W.T., 2002. Water Island Formation, U.S. Virgin Islands: a new look at the original primitive island arc (PIA) suite of the Caribbean. 16 Caribbean Geological Conference, Barbados, Abstracts, p. 34.

Linares, E., Osadchy, P., Dovbnia, A., et al., 1985. Mapa Geológico de la República de Cuba. Scale 1:50 000. Academia de Ciencias de Cuba. 4 sheets. Marchesi, C., Proenza, J., Gervilla, F., Garrido, C.J., Melgarejo, J.C., Díaz-Martínez, R., Godard, M., 2003. New petrological and structural constraints on the origin of the MayaríBaracoa ophiolitic belt (eastern Cuba). Geophysical Research Abstracts, 5, 00278.

Marchesi, C., Garrido, C.J., Godard, M., Proenza, J.A., Gervilla, F., Blanco-Moreno, J., in press. Petrogenesis of highly depleted peridotites and gabbroic rocks from the MayaríBaracoa ophiolitic belts (eastern Cuba). Contributions to Mineralogy and Petrology.

Meffre, S., Aitchison, J.C., Crawford, A.J., 1996. Geochemical evolution and tectonic significance of boninites and tholeiites from Koh ophiolite, New Caledonia. Tectonics, 15, 67-83.

Metzger, E.P., Miller, R.B., Harper, G.D., 2002. Geochemistry and tectonic setting of the Ophiolitic Ingalls Complex, North Cascade, Washington: Implications for correlations of

Jurassic Cordilleran Ophiolites. The Journal of Geology, 110, 543-560.

Morimoto, N., Fabries, J., Ferguson, A.K., Ginzburg, I.V., Ross, M., Seifeit, F.A., Zussman, J., 1989. Nomenclature of pyroxenes. Canadian Mineralogist, 27, 143-156.

Pearce, J., Lippard, S., Roberts, S., 1984. Characteristics and tectonic significance of supra-subduction zone ophiolites. Geological Society of London, Special Publication, 16, 77-94.

Pearce, J.A., Peate, D.W., 1995. Tectonic implications of the composition of volcanic arc magmas: Annual Reviews of Earth and Planetary Sciences, 23, 251-285.

Pearce, J.A., van der Laan, S.R., Arculus, R.J., Murton, B.J., Ishii, T., Peate, D.W., Parkinson, I.J., 1992. Boninite and harzburgite form Leg 125 (Bonin-Mariana forearc): A case study of magma genesis during the initial stages of subduction. Proceedings Ocean Drilling Program Science Results, 125, 623-659.

Pindell, J.L., Barrett, S.F., 1990. Geological evolution of the Caribbean region: a plate tectonic perspective. In: Dengo, G., Case, J.E. (eds.). The Caribbean. Decade of North American Geology, Boulder, Colorado, Geological Society of America, Volume H, 404-432.

Proenza, J., Gervilla, F., Melgarejo, J.C., Bodinier, J.L., 1999a. Al- and Cr- rich chromitites from the Mayarí-Baracoa Ophiolitic Belt (eastern Cuba): consequence of interaction between volatile-rich melts and peridotite in suprasubduction mantle. Economic Geology, 94, 547-566.

Proenza, J., Gervilla, F., Melgarejo, J.C., 1999b. La Moho Transition Zone en el Macizo Ofiolítico Moa-Baracoa: un ejemplo de interacción magma/peridotita. Revista de la Sociedad Geológica de España, 12, 309-327.

Proenza, J.A., Melgarejo, J.C., Gervilla, F., Rodríguez-Vega, A., Díaz-Martínez, R., Ruiz-Sánchez, R., Lavaut, W., 2003. Coexistence of Cr- and Al-rich ophiolitic chromitites in a small area: the Sagua de Tánamo district, Eastern Cuba. In: Eliopoulos et al. (eds.). Mineral Exploration and

Sustainable Development. Rotterdam Netherlands, Millpress, 1, 631-634.

Pushcharovsky, Yu. et al., 1988. Geologic Map of the Republic of Cuba, Scale 1:250 000. Moscow. Cuban and USSR Academy of Sciences, 42 sheets.

Quintas, F., 1988. Características estratigráficas y estructurales del complejo ofiolítico y eugeosinclinal de la cuenca del Río Quibiján, Baracoa. Minería y Geología, 6, 11-22.

Quintas, F., 1989. Análisis estratigráfico y paleogeografía del Cretácico superior y del Paleógeno de la provincia de Guantánamo y áreas cercanas. Doctoral thesis. Instituto Superior

Minero Metalúrgico de Moa., Holguín, Cuba, 161 pp.

Quintas, F., Hernández, M., Campos, M., 1994. Asociaciones estructuro-formacionales del Mesozoico en Cuba Oriental y La Española. Minería y Geología, 11, 3-9.

Shervais, J.W., 1982. Ti-V plots and the petrogenesis of modern and ophiolitic lavas. Earth Planetary Science Letters, 59, 101-118.

Simon, G., Kesler, S., Russel, N., Hall, C.M., Bell, D., Piñero, E., 1999. Epithermal gold mineralization in an old volcanic arc: the Jacinto deposit, Camagüey district, Cuba. Economic

Geology, 94, 487-506.

Staudigel, H., Albarede, F., Blichert-Toft, J., Edmond, J., McDonough, W.F., Jacobsen, S.B., Keeling, R., Langmuir, C.H., Nielsen, R.L., Plank, T., Rudnick, R., Shaw, H.F., Shirey, S.B., Veizer, J., White, W., 1998. Geochemical Earth Reference Model GERM: description of the initiative. Chemical Geology, 145, 153-159.

Steiger, R. H., Jager, E., 1977. Subcommission on geochronology: Convention on the use of decay constants in geo- and cosmochronology. Earth and Planetary Science Letters, 36, 359-363.

Stern, R.J., Morris, J., Bloomer, S.H., Hawkins, J.W., 1991. The source of the subduction component in convergent margin magmas: trace element and radiogenic isotope evidence

from Eocene boninites, Mariana forearc. Geochimica et Cosmochimica Acta, 55, 1467-1481.

Sun, S.-S., McDonough, W.F., 1989. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In: Saunder, A.D., Norry, M.J. (eds.).

Magmatism in the ocean basins. Geological Society Special Publication, 42, 313-345.

Torrez, M., Fonseca, E., 1990. Características geológicas petrológicas del contacto entre la asociación ofiolítica y el arco volcánico en Moa-Baracoa. Boletín de Geociencias, Centro Universitario de Pinar del Río, Cuba, 1, 12-19.

White, R.V., Tarney, J., Kerr, A.C., Saunders, A.D., Kempton, P.D., Pringle, M.S., Klaver, G.T., 1999. Modification of an oceanic plateu, Aruba, Dutch Caribbean: implications for the generation of continental crust. Lithos, 46, 43-68.

Wood, D.A., 1980. The application of a Th-Hf-Ta diagram to problems of tectonomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the Bristish Tertiary volcanic province. Earth and Planetary Science Letters, 50, 11-30.

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2006-01-11

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