Abstract
This paper addresses the composition, geochemistry, isotopic characteristics, and age of rocks from the Carter Seamount of the Grimaldi seamount group at the eastern margin of the Central Atlantic. The age of the seamount was estimated as 57–58 Ma. Together with other seamounts of the Grimaldi system and the Nadir Seamount, it forms a “hot line” related to the Guinea Fracture Zone, which was formed during the late Paleocene pulse of volcanism. The Carter Seamount is made up of olivine melilitites, ankaramites, and analcime-bearing nepheline tephrites, which are differentiated products of the fractional crystallization of melts similar to an alkaline ultramafic magma. The volcanics contain xenoliths entrained by melt at different depths from the mantle, layer 3 of the oceanic crust, which was formed at 113–115 Ma, and earlier magma chambers. The rocks were altered by low-temperature hydrothermal solutions. The parental melts of the volcanics of the Carter Seamount were derived at very low degrees of mantle melting in the stability field of garnet lherzolite at depths of no less than 105 km. Anomalously high Th, Nb, Ta, and La contents in the volcanics indicate that a metasomatized mantle reservoir contributed to the formation of their primary melts. The Sr, Pb, and Nd isotopic systematics of the rocks show that the composition of the mantle source lies on the mixing line between two mantle components. One of them is a mixture of prevailing HIMU and the depleted mantle, and the other is an enriched EM2-type mantle reservoir. These data suggest that the formation of the Carter Seamount volcanics was caused by extension-related decompression melting in the Guinea Fracture Zone of either (1) hot mantle plume material (HIMU component) affected by carbonate metasomatism or (2) carbonated basic enclaves (eclogites) ubiquitous in the asthenosphere, whose isotopic characteristics corresponded to the HIMU and EM2 components. In the former case, it is assumed that the melt assimilated during ascent the material of the metasomatized subcontinental mantle (EM2 component), which was incorporated into the oceanic lithospheric mantle during rifting and the breakup of Pangea.
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Battey, M.H. and Pring, A., Mineralogy for Students, London: Longman, 1997.
Bertrand, H., Feraud, G., and Mascle, J., Alkaline Volcano of Paleocene Age on the Southern Guinean Margin: Mapping, Petrology, 40Ar/39Ar Laser Probe Dating, and Applications for the Evolution for the Eastern Equatorial Atlantic, Mar. Geol., 1993, vol. 114, nos. 3/4, pp. 261–262.
Bonadiman, C., Beccaluva, L., Coltorti, M., and Siena, F., Kimberlite-Like Metasomatism and “Garnet Signature” in Spinel-Peridotite Xenoliths from Sal, Cape Verde Archipelago: Relics of a Subcontinental Mantle Domain within the Atlantic Oceanic Lithosphere?, J. Petrol., 2005, vol. 46, no. 12, pp. 2465–2493.
Bortnikov, N.S., Sharkov, E.V., Bogatikov, O.A., et al., Finds of Young and Ancient Zircons in Gabbroids of the Markov Deep, Mid-Atlantic Ridge, 5°30.6′–5°32.4′N (Results of SHRIMP-II U-Pb Dating): Implication for Deep Geodynamics of Modern Oceans, Dokl. Earth Sci., 2008, vol. 421, no. 2, pp. 859–866.
Brey, G.P., Bulatov, V.K., Girnis, A.V., and Lahaye, Y., Experimental Melting of Carbonated Peridotite at 6–10 GPa, J. Petrol., 2008, vol. 49, pp. 797–821.
Chernysheva, E.A. and Belozerova, O.Yu., Composition of Mantle Xenoliths from Melilitites and Evolution of Primary Alkaline Melt in the Nizhnesayanskii Carbonatite Complex, Geochem. Int. (Engl. Transl.), 2000, vol. 38, pp. 713–716.
Chernysheva, E.A. and Kostrovitskii, S.I., Olivine Melilitites of the Kimberlite and Carbonatite Associations in Dikes and Diatremes of Eastern Siberia, Geochem. Int., 1998, vol. 36, pp. 1100–1108.
Chernysheva, E.A., Belozerova, O.Yu., and Kostrovitskii, S.I., Cr-Spinellids from Olivine Melilitites of the Carbonatite Formation, Dokl. Earth Sci., 1999, vol. 365, pp. 260–263.
Cohen, R.S. and O’Nions, R.K., Identification of Recycled Continental Material in the Mantle from Sr, Nd and Pb Isotope Investigations, Earth Planet. Sci. Lett., 1982, vol. 61, pp. 73–84.
Corfu, F., Hanchar, J.M., Hoskin, P.W.O., and Kinny, P., Atlas of Zircon Textures, Rev. Mineral. Geochem, 2003, vol. 53, pp. 468–500.
Dasgupta, R., Hirschmann, M.M., and Stalker, K., Immiscible Transition from Carbonate-Rich to Silicate-Rich Melts in the 3 GPa Melting Interval of Ecologite + CO2 and Genesis of Silica-Undersaturated Ocean Island Lavas, J. Petrol., 2006, vol. 47, pp. 647–671.
Dasgupta, R., Hirschmann, M.M., and Smith, N.D., Partial Melting Experiments of Peridotite + CO2 and Genesis of Alkalic Ocean Island Basalts, J. Petrol., 2007, vol. 48, pp. 2093–2124.
Davidson, J. and Bohrson, W.A., Shallow-Level Processes in Ocean-Island Magmatism: Editorial, J. Petrol., 1998, vol. 39, pp. 799–801.
Doucelance, R., Escrig, S., Moreira, M., et al., Pb-Sr-He and Trace Element Geochemistry of the Cape Verde Archipelago, Geochim. Cosmochim. Acta, 2003, vol. 67, pp. 3717–3733.
Eiler, J.M., Schiano, J.M., Kitchen, N., and Stolper, E.M., Oxygen-Isotope Evidence for Recycled Crust in the Sources of Mid-Ocean-Ridge Basalts, Nature, 2000, vol. 403, pp. 530–534.
Ellam, R.M., Lithospheric Thickness as a Control on Basalt Geochemistry, Geology, 1992, vol. 20, pp. 153–156.
Feraud, G., York, D., Mevel, C., Cornen, G., et al., Additional 40Ar/39Ar Dating of the Basement and Alkaline Volcanism of Gorringe Bank (Atlantic Ocean), Earth Planet. Sci. Lett., 1986, vol. 79, pp. 255–269.
Fraser, K.J., Hawkesworth, C.J., Erlank, A.J., et al., Sr, Nd and Pb Isotope and Minor Element Geochemistry of Lamproites and Kimberlites, Earth Planet. Sci. Lett., 1985, vol. 76, pp. 57–70.
General Bathymetric Chart of the Oceans (GEBCO), Ottawa: Canad. Hydrogr. Serv., 2004.
Gerbode, C. and Dasgupta, R., Carbonate-Fluxed Melting of MORB-Like Pyroxenite at 2.9 GPa and Genesis of HIMU Ocean Island Basalts, J. Petrol., 2010, vol. 51, no. 10, pp. 2067–2088.
Gerlach, D.C., Cliff, R.A., Davies, G.R., et al., Magma Sources of the Cape Verde Archipelago: Isotopic and Trace Elements Constraints, Geochim. Cosmochim. Acta, 1988, vol. 52, pp. 2979–2992.
Gibson, S.A., Thompson, R.N., Leonardos, O.H., et al., The Limited Extent of Plume-Lithosphere Interactions during Continental Flood-Basalt Genesis: Geochemical Evidence from Cretaceous Magmatism in Southern Brazil, Contrib. Mineral. Petrol., 1999, vol. 137, pp. 147–169.
Gudfinnsson, G. and Presnall, D.C., Continuous Gradations among Primary Carbonatitic, Kimberlitic, Melilititic, Basaltic, Picritic, and Komatiitic Melts in Equilibrium with Garnet Lherzolite at 3–8 GPa, J. Petrol., 2005, vol. 46, pp. 1645–1659.
Hart, S.R., A Large Scale Isotope Anomaly in the Southern Hemisphere Mantle, Nature, 1984, vol. 309, pp. 753–757.
Hart, S.R., Heterogeneous Mantle Domains: Signatures, Genesis and Mixing Chronology, Earth Planet. Sci. Lett., 1988, vol. 90, pp. 273–296.
Hawkesworth, C.J., Kempton, P.D., Rogers, R.M., et al., Continental Mantle Lithosphere and Shallow Level Enrichments Processes in the Earth’s Mantle, Earth Planet. Sci. Lett., 1990, vol. 96, pp. 256–268.
Hayes, D.E. and Rabinowitz, P.D., Mesozoic Magnetic Lineations and the Magnetic Quiet Zone of Northwest Africa, Earth Planet. Sci. Lett., 1975, vol. 28, pp. 105–115.
Hekinian, R., Bonte, P., Dudley, W., et al., Volcanics from the Sierra Leone Rise, Nature, 1978, vol. 275, pp. 536–538.
Heller, D. and Marquart, G., An Admittance Study of the Reykjanes Ridge and Elevated Plateaux between the Charlie Gibbs and Senja Fracture Zones, Geophys. J. Int., 2002, vol. 148, pp. 65–76.
Hill, R. and Roeder, P., The Crystallization of Spinel from Basaltic Liquid as a Function of Oxygen Fugacity, J. Geol., 1974, vol. 82, pp. 709–729.
Hirose, K., Partial Melt Compositions of Carbonated Peridotite at 3 GPa and Role of CO2 in Alkali-Basalt Magma Generation, Geoph. Res. Let, 1997, vol. 24, pp. 2837–2840.
Hirschmann, M.M. and Stolper, E.M., A Possible Role for Garnet Pyroxenite in the Origin of the “Garnet Signature” in MORB, Contrib. Mineral. Petrol., 1996, vol. 124, pp. 185–208.
Hoernle, K., Tilton, G., and Schminke, H-U., Sr-Nd-Pb Isotopic Evolution of Gran Canaria: Evidence for Shallow Enriched Mantle beneath the Canary Islands, Earth Planet. Sci. Lett., 1991, vol. 106, pp. 44–64.
Hoernle, K., Zhang, Y., and Graham, D., Seismic and Geochemical Evidence for Large-Scale Mantle Upwelling beneath the Eastern Atlantic and Western and Central Europe, Nature, 1995, vol. 374, pp. 34–39.
Hofmann, A.W., Chemical Differentiation of the Earth: The Relationship between Mantle, Continental Crust and Ocean Crust, Earth Planet. Sci. Lett., 1988, vol. 90, pp. 297–314.
Hofmann, A.W., Mantle Geochemistry: the Message from Oceanic Volcanism, Nature, 1997, vol. 385, pp. 219–229.
Hofmann, A.W. and White, W.M., Mantle Plumes from Ancient Oceanic Crust, Earth Planet. Sci. Lett., 1982, vol. 57, pp. 421–436.
Holm, P.M., Christensen, B.P., Hansen, L., et al., Sampling the Cape Verde Mantle Plume: Evolution of Melt Compositions on Santo Antao, Cape Verde Islands, J. Petrol., 2006, vol. 47, no. 1, pp. 145–189.
Hoskin, P.W.O. and Schaltegger, U., The Composition of Zircon and Igneous and Metamorphic Petrogenesis, Rev. Mineral. Geochem., 2003, vol. 53, pp. 27–62.
Huang, S. and Frey, F., Recycled Oceanic Crust in the Hawaiian Plume: Evidence from Temporal Geochemical Variations within the Koolau Shield, Contrib. Mineral. Petrol., 2005, vol. 149, pp. 556–575.
Ito, E., White, W.M., and Gopel, C., The O, Sr, Nd and Pb Isotope Geochemistry of MORB, Chem. Geol., 1987, vol. 62, pp. 157–176.
Jackson, M.G. and Dasgupta, R., Compositions of HIMU, EM1, and EM2 from Global Trends between Radiogenic Isotopes and Major Elements in Ocean Island Basalts, Earth Planet. Sci. Lett., 2008, vol. 276, pp. 175–186.
Janney, P.E., Le Roex A.P., Carlson R.W., Viljoen K.S. A Chemical and Multi-Isotope Study of the Western Cape Olivine Melilitite Province, South Africa: Implications for the Sources of Kimberlites and the Origin of the HIMU Signature in Africa, J. Petrol., 2002, vol. 43, no. 12, pp. 2339–2370.
Jones, E.J.W., Fracture Zones in the Equatorial Atlantic and the Breakup of Western Pangea, Geology, 1987, vol. 15, pp. 533–536.
Jones, E.J.W., Goddard, D.A., Mitchell, J.G., and Banner, F.T., Lamprophyric Volcanism of Cenozoic Age on the Sierra-Leone Rise: Implication for Regional Tectonics and the Stratigraphic Time Scale, Mar. Geology, 1991, vol. 99, pp. 19–28.
Kashintsev, G.L., Glubinnye porody okeanov (Deep Oceanic Rocks), Moscow: Nauka, 1991.
Kharin, G.S., Magmatic Rocks of the Submarine Sierra Leone Rise, Okeanologiya, 1988, vol. 28, no. 1, pp. 82–88.
Kokfelt, T.F., Holm, P.M., Hawkesworth, C.J., and Peate, D.W., A Lithospheric Mantle Source for the Cape Verde Island Magmatism: Trace Element and Isotopic Evidence from the Island Fogo, Mineral. Mag., 1998, vol. 62A, pp. 801–820.
Kumar, N. and Embley, R.W., Evolution and Origin of Ceara Rise: An Aseismic Rise in the Western Equatorial Atlantic, Geol. Soc. Am. Bull., 1977, vol. 88, pp. 683–694.
Lancelot, Y., Seibold, E., Cepek, P., et al., Site 366: Cape Verde Basin, Init. Rept. DSDP, 41, 21–162 (1978).
Leake, B.E., Woolley, A.R., Arps, C.E.S., et al., Nomenclature of Amphiboles. Report of the Subcommittee on Amphiboles of the International Mineralogical Association Commission on New Minerals and Mineral Names, Eur. J. Mineral., 1997, vol. 9, pp. 623–651.
Loubet, M., Sassi, R., and Donato, R., Mantle Heterogeneities: A Combined Isotope and Trace Element Approach and Evidence for Recycled Continental Crust Materials in Some OIB Sources, Earth Planet. Sci. Lett., 1988, vol. 89, pp. 299–315.
Lundstrom, C.C., Gill, J., and Williams, Q., A Geochemically Consistent Hypothesis for MORB Generation, Chem. Geol., 2000, vol. 162, pp. 105–126.
Magmaticheskie gornye porody (Igneous Rocks), Bogatikov, O.A., Ed., Moscow: Nauka, 1983.
Marques, L.S., Mabel, N.C., Ulbrich, E.R., and Colombo, G.T., Petrology, Geochemistry and Sr-Nd Isotopes of the Trindade and Martin Vaz Volcanic Rocks Southern Atlantic Ocean, J. Volcanol. Geoth. Res., 1999, vol. 93, pp. 191–216.
Mazarovich, A.O., The Structure and History of the Volcanic Islands and Seamounts of the Tropical Atlantic, Geotectonics 1998, vol. 32, pp. 296–307].
Mazarovich, A.O., Geologicheskoe stroenie Tsentral’noi Atlantiki: razlomy, vulkanicheskie sooruzheniya i deformatsii okeanskogo dna (Geological Structure of the Central Atlantic: Faults, Volcanic Edifices, and Deformations of the Ocean Floor), Moscow: Nauchnyi Mir, 2000.
Mazarovich, A.O., Frikh-Khar, D.I., Kogarko, L.N., et al., Tektonika i magmatizm ostrovov Zelenogo Mysa (Tectonics and Magmatism of the Cape Verde Islands), Moscow: Nauka, 1990.
McKenzie, D. and O’Nions, R.K., Mantle Reservoirs and Ocean Island Basalts, Nature, 1983, vol. 393, pp. 229–231.
Morgan, W.J., Hotspot Tracks and the Opening of the Atlantic and Indian Ocean, in The Sea, Emiliani, C.,. Ed., New York: Wiley-Chichester, 1981, vol. 7, pp. 443–487.
Morimoto, N., Fabries, J., and Ferguson, A.K., Nomenclature of Pyroxenes, Am. Mineral., 1988, vol. 73, nos. 9–10, pp. 1123–1134.
Niu, Y. and Batiza, R., Trace Element Evidence from Seamounts for Recycled Oceanic Crust in the Eastern Pacific Mantle, Earth Planet. Sci. Lett., 1997, vol. 148, pp. 471–483.
Niu, Y. and O’Hara, M.J., Origin of Ocean Island Basalts: A New Perspective from Petrology, Geochemistry, and Mineral Physics Consideration, J. Geophys. Res., 2003, vol. 108, pp. 2002–2048.
Panaev, V.A. and Mitulov, S.N., Seismostratigrafiya osadochnogo chekhla Atlanticheskogo okeana (Sesimostratigraphy of the Sedimentary Cover of the Atlantic Ocean), Moscow: Nedra, 1993.
Peyve, A.A. and Skolotnev, S.G., Alkali Volcanism of the Bathymetrists Seamounts Chain (Central Atlantic): Characteristics and Comparison, Dokl. Earth Sci., 2009, vol. 425, no. 1, pp. 243–248.
Pilet, S., Baker, M.B., and Stolper, E.M., Metasomatized Lithosphere and the Origin of Alkaline Lavas, Science, 2008, vol. 320, pp. 916–919.
Pilot, J., Werner, C.D., Haubrich, F., and Baumann, N., Paleozoic and Proterozoic Zircons from the Mid-Atlantic Ridge, Nature, 1998, vol. 393, pp. 676–679.
Pushcharovskii, Yu.M., Skolotnev, S.G., Peyve, A.A., et al., Geologiya i metallogeniya Sredinno-Atlanticheskogo khrebta, 5–7s.sh (Geology and Metallogeny of the Mid-Atlantic Ridge, 5-7°N), Moscow: GEOS, 2004.
Putirka, K., Melting Depths and Mantle Heterogeneity beneath Hawaii and the East Pacific Rise: Constraints from Na/Ti and Rare Earth Element Ratios, J. Geophys. Res., 1999, vol. 104, pp. 2817–2829.
Ritsema, J., Ni, S., Helmberger, D.V., and Crotwell, H.P., Evidence for Strong Shear Velocity Reductions and Velocity Gradients in the Lower Mantle beneath Africa, Geophys. Res. Lett., 1998, vol. 25, pp. 4245–4248.
Sandwell, D.T. and Smith, W.H.F., Marine Gravity Anomaly from Geosat and ERS-1 Satellite Altimetry, J. Geophys. Res., 1997, vol. 102, pp. 10039–10054.
Schilling, J.G., Hanan, B.B., MacCully B., et al. Influence of the Sierra Leone Mantle Plume on the Equatorial Mid-Atlantic Ridge: Nd-Sr-Pb Isotopic Study, J. Geophys. Res., 1994, vol. 99, pp. 12005–12028.
Shulyatin, O.G., Andreev, S.I., Belyatskii, B.V., and Trukhalev, A.I., Structural-Tectonic Position and Age of the Plutonic Mafic-Ultramafic Complexes of MAR, in 60 let v Arktike, Antarktike i Mirovom okeane (60 Years in Arctic, Antarctica, and World Ocean), St. Petersburg: VNI-IOkeangeologiya, 2008, pp. 392–408.
Siebel, W., Becchiob, R., Volkerc, F., Hansene, M.A.F., et al., Trinidade and Martin Vaz Islands, South Atlantic: Isotopic (Sr, Nd, Pb) and Trace Element Constraints on Plume Related Magmatism, Tectonophysics, 2000, vol. 13, pp. 79–103.
Skolotnev, S.G., Turko, N.N., Sokolov, S.Yu., et al., New Data on the Geological Structure of the Junction of the Cape Verde Plateau, Cape Verde Abyssal Plain, and Bathymetrists Seamounts (Central Atlantic Ocean), Dokl. Earth Sci., 2007, vol. 416, no. 7, pp. 1037–1041.
Skolotnev, S.G., Kolodyazhnyi, S.Yu., Tsukanov, N.V., et al., Neotectonic Morphotructures in the Junction Zone of the Cape Verde Rise and Cape Verde Abyssal Plain, Central Atlantic, Geotectonics, 2009, vol. 42, pp. 51–66.
Skolotnev, S.G., Bel’tenev, V.E., Lepekhina, E.N., and Ipat’eva, I.S., Younger and Older Zircons from Rocks of the Oceanic Lithosphere in the Central Atlantic and Their Geotectonic Implications, Geotectonics, 2010, vol. 44, pp. 462–492.
Sun, S.-S. and McDonough, W.F., Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes, in Magmatism in the Ocean Basins, Saunders, A.D. and Norey, M.J., Geol. Soc. London, Sp. Publ., 1989, vol. 42, pp. 313–345.
Weaver, B.L., The Origin of Ocean Island Basalt End-Member Compositions: Trace Elements and Isotopic Constraints, Earth Planet. Sci. Lett., 1991, vol. 104, pp. 381–397.
Weaver, B.L., Wood, D.A., Tarney, J., and Joron, J.L., Role of Subducted Sediments in the Genesis of Ocean-Island Basalts: Geochemical Evidence from South Atlantic Ocean Islands, Geology, 1986, vol. 14, pp. 275–278.
White, R.S., Detrick, R.S., Mutter, J.S., et al., New Seismic Images of Oceanic Crustal Structure, Geology, 1990, vol. 18, pp. 462–465.
Williams, I.S., Applications of Microanalytical Techniques to Understanding Mineralizing Processes, Rev. Econ. Geol., 1998, vol. 7, pp. 1–35.
Zakrutkin, V.V., Metamorphic Evolution of Amphiboles, Zap. Vses. Mineral. O-va, 1968, 97, pp. 13–23.
Zindler, A. and Hart, S.R., Chemical Geodynamics, Earth Planet. Sci. Lett., 1986, vol. 14, pp. 493–571.
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Original Russian Text © S.G. Skolotnev, V.V. Petrova, A.A. Peyve, 2012, published in Petrologiya, 2012, Vol. 20, No. 1, pp. 66–94.
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Skolotnev, S.G., Petrova, V.V. & Peyve, A.A. Origin of submarine volcanism at the eastern margin of the central atlantic: Investigation of the alkaline volcanic rocks of the carter seamount (Grimaldi Seamounts). Petrology 20, 59–85 (2012). https://doi.org/10.1134/S086959111106004X
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DOI: https://doi.org/10.1134/S086959111106004X