Abstract
Mantle-derived peridotites sampled on the seafloor at 23° N along the MidAtlantic Ridge during the Hydrosnake and R.V. Akademic Mstislav Keldysh cruises show evidence of minor magmatic intrusion that produced millimetre to centimetre thick gabbroic dikelets. The nature of the intruding magma and the time relationships between intrusion events and tectonic evolution of the host peridotites is inferred from the mineralogy and textural features of veins cutting the peridotites. The occurrence of Fe-Ti-rich minerals and of zircon in the veins suggests an evolved, basaltic composition of the fluid. Pyroxene-rich, plagioclase-free veins probably represent pyroxenite dikelets inside the peridotites. In all cases, melt intrusion followed ductile deformation affecting the mantle-derived ultramafics. These observations fit with a model in which gabbroic intrusions are emplaced in mantle rocks at shallow depths beneath the ridge axis.
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References
Agrinier, P., Mével, C. and Girardeau, J., 1988. Hydrothermal alteration of the peridotites cored at the ocean/continent boundary of the Iberian margin: petrologic and stable isotope evidence. In: G. Boillot, E.L. Winterer et al. (Editors), Proc. of the ODP, Scientific Results, 103: 225–234.
Aumento, F. and Loubat, H., 1971. The Mid-Atlantic Ridge near 45°N. XVI. Serpentinized ultramafic intrusions. Canad. Journ. Earth Sci., 8: 631–663.
Benn, K., Nicolas, A. and Reuber, I., 1988. Mantle-crust transition zone and origin of wehrlitic magmas: evidence from the Oman ophiolite. Tectonophysics, 151: 75–85.
Bergès, J.P.,1989. Modélisation gravimétrique de la ride Médio-Atlantique: mur Ouest et Snake Pit à la latitude 23°20′N, Rapport DEA, Université de Paris VI.
Bloomer, S.H., Natland, J.H. and Fisher, R.L., 1989. Mineral relationships in gabbroic rocks from fracture zones of Indian Ocean ridges: evidence for extensive fractionation, parental diversity, and boundary-layer recrystallization. In: A.D. Saunders and M.J. Norry (Editors), Magmatism in the Ocean Basins. Geol. Soc. London Spec. Publ., 42: 107–124.
Blundy, J.D. and Holland, T.J.B., 1990. Calcic amphibole equilibria and a new amphibole-plagioclase geothermometer. Contrib. Mineral. Petrol., 104: 208–224.
Bonatti, E., Honnorez, J., Kirst, P. and Radicati, F., 1975. Metagabbros from the Mid-Atlantic Ridge at 6°N: Contact-hydrothermal-dynamic metamorphism beneath the axial valley. Journ. Geol., 83: 61–78.
Bonatti, E. and Michael, P.J., 1989. Mantle peridotites from continental rifts to ocean basins to subduction zones. Earth Planet. Sci. Lett., 91: 297–311.
Bonatti, E., Peyve, A., Kepezhinskas, P., Kurentsova, N., Seyler, M., Skolotnev, S., and Udintsev, G., 1992. Upper mantle heterogeneity below the Mid-Atlantic Ridge, 0°-15°N. J. Geophys. Res., 97: 4461–4476.
Boudier, F., 1979. Microstructural studies of three peridotite samples drilled at the western margin of the midAtlantic Ridge. Init. Repts. of the DSDP 45: 603–608.
Bougault, H., Cande, S.C., et al., 1985. Initial Reports of the Deep Sea Drilling Project, 82, Washington.
Bougault, H., Charlou, J. L., Fouquet, Y. and Needham, H.D., 1990. Campagne RIDELENTE, structure de la dorsale Atlantique, hétérogenité du manteau et hydrothermalisme. Oceanol. Acta, Vol. Spec., 10: 366–381.
Brown, G.M., 1957. Pyroxenes from the early and middle stages of fractionation of the Skaergaard intrusion, East Greenland. Mineral. Mag., 31: 511–543.
Brown, G.M. and Vincent, E.A., 1963. Pyroxenes from the late stages of fractionation of the Skaergaard intrusion. J. Petrol., 4: 175–197.
Cannat, M., 1993. Emplacement of mantle rocks in the seafloor at mid-ocean ridges. J. Geophys. Res., 98: 4163–4172.
Cannat, M., Bideau, D. and Bougault, H., 1992. Serpentinized peridotites and gabbros in the Mid-Atlantic Ridge axial valley at 15°37′N and 16°52′N. Earth Planet. Sci. Lett., 109: 87–106.
Cannat, M., Juteau, T. and Berger, E., 1991. Petrostructural analyses of the leg 109 serpentinized peridotites. In: R.S. Detrick, J. Honnorez, W.B. Bryan, T. Juteau, et al. (Editors), Proc. of the ODP, Scientific Results, 109: 47–56.
Casey, J.F., 1986. Ultramafic rocks from the MAR at 23° N: evidence for high temperature hydration and high temperature-low to moderate stress deformation of mantle tectonites beneath the median valley. Eos, 67: 1214.
Ceuleneer, G., Nicolas, A. and Boudier, F., 1988. Mantle flow patterns at an oceanic spreading centre: the Oman peridotites record. Tectonophysics, 151: 1–26.
Cormier, M.H., Detrick, R.S. and Purdy, G.M., 1984. Anomalously thin crust in oceanic fracture zones; new seismic constraints from the Kane fracture zone. J. Geophys. Res., 89: 10244–10266.
Detrick, R.S., Fox, P. J., Kastens, K., Ryan, WB.F., Mayer, L., Karson, J. and Pockalny, R., 1984. A SeaBeam survey of the Kane fracture zone and adjacent Mid-Atlantic ridge rift valley. Eos, 65: 1006.
Detrick, R.S., Honnorez, J., Bryan, WB., Juteau, T., et al., 1988. Proceeding of the Ocean Drilling Program, Init. Repts., 106/109, College Station, TX.
Dick, H.J.B., 1989. Abyssal peridotites, very slow spreading ridges and ocean ridge magmatism, In: A.D. Saunders and M.J. Norris (Editors), Magmatism in the Ocean Basins. Geol. Soc. London Spec. Publ., 42: 71–105.
Dick, H.J.B., Fisher, R.L. and Bryan, WB., 1984. Mineralogic variability of the uppermost mantle along midocean ridges. Earth Planet. Sci. Lett., 69: 88–106.
Droop, G.T.R., 1987. A general equation for estimating Fe3+ concentrations in ferromagnesian silicates and oxides from microprobe analyses, using stoichiometric criteria. Mineral. Magazine, 51: 431–435.
Dungan, M.A., 1979. A microprobe study of antigorite and some serpentine pseudomorphs. Canad. Mineral., 17: 771–784.
Engel, C.G. and Fisher, R.L., 1975. Granitic to ultramafic rock complexes of the Indian Ocean ridge system, western Indian Ocean. Geol. Soc. Am. Bull., 86: 1553–1578.
Fisher, R.L., Dick, H.J.B., Natland, J.H. and Meyer, P.S., 1986. Mafic-ultramafic suites of the slowly spreading Southwest Indian Ridge: PROTEA exploration of the Antarctic plate boundary, 24°E-47°E. Ofioliti, 11: 147–178.
Fox, P.J. and Gallo, D.G., 1984. A tectonic model for ridge-transform-ridge plate boundaries: implications for the structure of the oceanic lithosphere. Tectonophysics, 104: 205–242.
Francis, T.G., 1981. Serpentinization faults and their role in the tectonics of slow-spreading ridges. J. Geophys. Res. 86: 11616–11622.
Fryer, P., Pearce, J.A., Stokking, L.B., et al., 1990. Proceeding of the Ocean Drilling Program. Init. Repts., 125, College Station, TX.
Gente, P., Zonenshain, L.P., Kuzmin, M., Lisitsin, A.P., Bodganov, Y.A. et Baranov, B.V., 1989. Géologie de l’axe de la dorsale médio-atlantique entre 23° et 26°N: résultats préliminaires de la 15eme campagne du N.O. Akademik Mtislav Keldysh (mars-avril 1988). C.R. Acad. Sci. Paris, 308: 1781–1788.
Gillis, K.M., Thompson, G., and Kelley, D.S.,1993. A view of the lower crustal component of hydrothermal systems at the Mid-Atlantic Ridge. J. Geophys. Res., 98: 19597–19619.
Hamlyn, P.R. and Bonatti, E., 1980. Petrology of mantle-derived ultramafics from the Owen Fracture Zone, Northwest Indian Ocean: implications for the nature of the oceanic upper mantle. Earth Planet. Sci. Lett., 48: 65–79.
Harper, G.D.,1984. The Josephine ophiolite. Geol. Soc. Am. Bull., 95: 1009–1026.
Hébert, R., Serri, G. and Hékinian, R., 1989. Mineral chemistry of ultramafic to gabbroic cumulates from the major oceanic basins and Northern Apennine ophiolites (Italy) — A comparison. Chem. Geol., 77: 183–207.
Juteau, T., Berger, E. and Cannat, M., 1990. Serpentinized, residual mantle peridotites from the M.A.R. Median valley, ODP Hole 670A (21°10′N, 45°02′W, Leg 109): primary mineralogy and geothermometry. In: R.S. Detrick, J. Honnorez, W.B. Bryan, T. Juteau, et al. (Editors), Proc. of the ODP, Scientific Results, 109: 27–45.
Karson, J.A., 1991. Seafloor spreading on the Mid-Atlantic Ridge: implications for the structure of ophiolites and oceanic lithosphere produced in slow-spreading environments. In: J. Malpas, M.J. Moores, A. Panayiotou and C. Xenophontos (Editors), Proc. Symp. Troodos 1987, Geol. Surv. Dep., Nicosia, Cyprus, pp. 547–555.
Karson, J.A. and Dick, H.J.B., 1983. Tectonics of ridge-transform intersections at the Kane fracture zone. Mar. Geophys. Res., 6: 51–98.
Karson, J.A., Collins, J.A. and Casey, J.F., 1984. Geologic and seismic velocity structure of the crust/mantle transition in the Bay of Islands ophiolite complex. J. Geophys. Res., 89: 6126–6138.
Karson, J.A., Thompson, G., Humphris, S.E., Edmond, J.M., Bryan, WB., Brown, J.R., Winters, A.T., Pockalny, R.A., Casey, J.F., Campbell, A.C., Klinkhammer, C., Palmer, M.R., Kinzler, R.J. and Sulanowska, M.M., 1987. Along axis variations in seafloor spreading in the MARK area. Nature, 328: 681–685.
Kirby, S.H.,1983. Rheology of the lithosphere. Rev. Geophys., 21: 1458–1483.
Kong, L.S.L., Detrick, R.S., Fox, P.J., Mayer, L.A. and Ryan, W.B.F., 1988. The morphology and tetconics of the Mark area from SeaBeam and SeaMark I observations (Mid-Atlantic Ridge 23° N). Mar. Geophys. Res., 10: 59–90.
Leake, B.E., 1965. The relationship between composition of calciferous amphiboles and grade of metamorphism, In: W.S. Pitcher and G.W. Flinn (Editors), Controls of metamorphism, Edimburgh and London, Oliver & Boyd, pp. 299–318.
Leake, B.E.,1978. Nomenclature of amphiboles. Can. Mineral.,16: 501–520.
Liou, J.G., Kuniyoshi, S. and Ito, K., 1974. Experimental studies of the phase relations between greenshist and amphibolite in a basaltic system. Am. J. Sci., 274: 613–632.
Manning, C.E. and Bird, D.K., 1986. Hydrothermal clinopyroxenes of the Skaergaard intrusion. Contrib. Mineral. Petrol., 92: 437–447.
Melson, W.G., Rabinowitz, P.D., et al., 1978. Initial Reports of the Deep Sea Drilling Project, 45, Washington.
Mercier, J.-C. C. and Nicolas, A., 1975. Textures and fabrics of upper-mantle peridotites as illustrated by xenoliths from basalts. J. Petrol., 16: 454–487.
Mével, C., Auzende, J.M., Cannat, M., Dubois, J., Fouquet, Y, Gente, P., Donval, J.P., Grimaud, D., Karson, J.A., Segonzac, M. and Stievenard, M., 1988. HYDROSNAKE 1988: submersible study of seafloor spreading in the MARK area, abstract) AGU, EOS, 69: 1439.
Mével, C., Cannat, M., Pascal, G., Marion, E., Auzende, J.M. and Karson, J.A., 1991. Emplacement of deep crustal and mantle rocks on the west median valley wall of the MARK area (MAR, 23°N). Tectonophysics, 190: 31–53.
Michael, P.J. and Bonatti, E., 1985. Peridotite composition from the North Atlantic: regional and tectonic variations and implications for partial melting. Earth Planet. Sci. Lett., 73: 91–104.
Morris, E. and Detrick, R.S., 1991. Three-dimensional analysis of gravity anomalies in the MARK area (MAR, 23°N). J. Geophys. Res., 96: 4355–4366.
Nicolas, A. and Jackson, M., 1982. High temperature dikes in peridotites: origin by hydraulic fracturing. J. Petrol., 23: 568–582.
Nicolas, A. and Poirier, J.P.,1976. Crystalline plasticity and solid state flow in metamorphic rocks, Wiley, London.
Nicolas, A. and Prinzhofer, A., 1983. Cumulative or residual origin for the transition zone in ophiolites: structural evidence. J. Petrol., 24: 188–206.
Nicolas, A., Reuber, I. and Benn, K., 1988. A new magma chamber model based on structural studies in the Oman ophiolite. Tectonophysics, 151: 87–105.
Nwe, Y.Y., 1976. Electron probe studies of the earlier pyroxenes and olivines from the Skaergaard intrusion, East Greenland. Contrib. Mineral. Petrol., 55: 105–126.
Phillips, J.D., Thompson, G., Bowen, V.T. and Von Herzen, R.P., 1968. Geophysical and geological study of the Mid-Atlantic Ridge. Trans. Amer. Geophys. Union, 49: 327–328.
Pockalny, R.A., Detrick, R.S. and Fox, P.J., 1988. Morphology and tectonics of the Kane transform from seabeam bathymetry data. J. Geophys. Res., 93: 3179–3193.
Prichard, H.M., 1979. A petrographic study of the process of serpentinization in ophiolites and ocean crust. Contrib. Mineral. Petrol., 68: 231–241.
Purdy, G.M. and Detrick, R.S., 1986. Crustal structure of the Mid-Atlantic Ridge at 23°N from seismic refraction studies. J. Geophys. Res., 91: 3739–3762.
Robinson, P., Spear, F.S., Schumaker, J.C., Laird, K., Klein, C., Evans, B.W. and Doolan, B.W, 1981. Phase relations of metamorphic amphiboles: natural occurrence and theory. In: D. Veblen (Editor), Amphiboles and other hydrous pyroboles-Mineralogy, MSA Rev. Mineral., 9B.
Rock, N.M.S. and Carroll, G.W, 1990. MINTAB: a general-purpose mineral recalculation and tabulation program for Macintosh microcomputers. Am. Mineral., 75: 424–430.
Rona, P.A., Widenfalk, L. and Boström, K., 1987. Serpentinized ultramafics and hydrothermal activity at the Mid-Atlantic Ridge crest near 15° N. J. Geophys. Res., 92: 1417–1427.
Schulz, N.J., Detrick, R.S. and Miller, S.P.,1988. Two and three dimensional inversions of magnetic anomalies in the MARK area (Mid-Atlantic Ridge 23°N). Mar. Geophys. Res., 10: 41–57.
Severinghaus, J.P. and Macdonald, K.C., 1988. High inside corners at ridge-transform intersections. Mar. Geophys. Res., 9: 353–367.
Sinton, J.M., 1979. Petrology of (alpine-type) peridotites from site 395, DSDP Leg 45. In: W.G. Melson, P.D. Rabinowitz et al. (Editors), Init. Repts. of the DSDP, 45: 595–601.
Sleep, N.H., 1975. Formation of ocean crust: some thermal constraints. J. Geophys. Res., 80: 4037–4042.
Spear, F.S., 1981. An experimental study of hornblende stability and compositional variability in amphibolite. Am., J., Sci., 281: 697–734.
Stakes, D., Mével, C., Cannat, M., and Chaput, T., 1991. Metamorphic stratigraphy of hole 735B. Proc. of the ODP, Scientific Results, 118: 153–180.
Tiezzi, L.J. and Scott, R.B., 1980. Crystal fractionation in a cumulate gabbro, Mid-Atlantic Ridge, 26° N. J. Geophys. Res., 85: 5438–5454.
Tucholke, B.E. and Schouten, H., 1988. Kane fracture zone. Mar. Geophys. Res., 10: 1–39.
Vieten, K. and Hamm, H.M., 1978. Additional notes “On the calculation of the crystal chemical formula of clinopyroxenes and their content of Fe3+ from microprobe analyses”. Neues Jahrb. Mineral. Monatshefte, 2: 71–83.
Wicks, F.J. and Whittaker, E.J.W., 1977. Serpentine texture and serpentinization. Can. Mineral., 13: 244–258.
Zonenshain, L.P., Kusmin, M.I., Lisitsin, A.P., Bogdanov, Yu.A. and Baranov, B.V., 1989. Tectonics of the Mid Atlantic rift valley between the TAG and MARK areas (26–24° N): evidence for vertical tectonism. Tectonophysics, 159: 1–23.
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Tartarotti, P., Cannat, M., Mevel, C. (1995). Gabbroic Dikelets in Serpentinized Peridotites from the Mid-Atlantic Ridge at 23°20’N. In: Vissers, R.L.M., Nicolas, A. (eds) Mantle and Lower Crust Exposed in Oceanic Ridges and in Ophiolites. Petrology and Structural Geology, vol 6. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-8585-9_3
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