Abstract
Major element, Ni, Mn and Ca electron microprobe analyses of olivine phenocrysts in one of the most primitive basalts from the FAMOUS area of the Mid-Atlantic Ridge, 527-1-1, reveal two different olivine populations, distinguished by their zoning characteristics. The often skeletal Group I olivines have zoning profiles with high forsterite, high Ni, low Mn, and low Ca cores. These profiles can be explained by low pressure crystallization from the 527-1-1 magma on cooling. The equant, often megacrystic Group II olivines also have high forsterite, low Mn cores, but the cores have low Ni compared to rims. Thus they are normally zoned with respect to Mg, Fe, and Mn but reversely zoned with respect to Ni. For example, Ni ranges from 1,700 ppm at Fo90.5 in the core to 2,100 ppm at Fo89.5 at the rim. In view of the published whole rock and mineral data of le Roex et al. (1981), the most likely explanation for these data is that the Group II olivines are xenocrysts assimilated from solidified “plagioclase-pyroxene” basalts through which the 527-1-1 basalt ascended. The diffusion rate of Ni and size of the xenocrystic olivines are used to calculate the residence time of the assimilated olivines in the magma. An alternative hypothesis would be a high pressure origin for the Group II olivines. This would be possible if future experiments show that with increasing pressure the partition coefficient for Ni decreases relative to the partition coefficient for Mg for a given bulk composition. Current evidence suggests this is unlikely. The data from 527-1-1 and other samples from the FAMOUS area require magmas with distinct Ni-MgO-FeO characteristics. In general, MORB from different ridge segments fall on distinct trends on plots of MgOvs. Ni as well as MgOvs. FeO. Calculation of the MgO and Ni contents of primary magmas suggests a mechanism by which such distinct trends could come about.
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References
Albarede F, Bottinga Y (1972) Kinetic disequilibrium in trace element partitioning between phenocrysts and host lava. Geochim Cosmochim Acta 36:141–156
Bence AE, Brande GJ, Indelicato GJ, Allen F (1980) Analysis of trace and minor elements in rock-forming minerals using an automated electron probe. In: Beaman RE, Ogilvie RE, Wittry DB (eds) Eighth Internat'l Congress X-ray Optics X-ray Microanalysis, pp 238–249
Bender JF, Hodges FN, Bence AE (1978) Petrogenesis of basalts from Project FAMOUS: Experimental study from 0–15 Kbar. Earth Planet Sci Lett 41:277–302
Bougault H, Hekinian R (1974) Rift valley in the Atlantic Ocean near 36° 50′N: Petrology and geochemistry of basaltic rocks. Earth Planet Sci Lett 24:249–261
Bryan WB, Moore JG (1977) Compositional variations of young basalts in the Mid-Atlantic Ridge rift valley near lat. 36° 49′N. Geol Soc Am Bull 88:556–570
Bryan WB, Thompson G, Michael PJ (1979) Compositional variation in a steady state zoned magma chamber: Mid-Atlantic Ridge at 36° 50′N. Tectonophysics 55:63–85
Clarke DB, O'Hara MJ (1979) Nickel, and the existence of high-MgO liquids in nature. Earth Planet Sci Lett 44:153–158
Crank J (1975) The Mathematics of Diffusion, 2nd Edit. Oxford Univ Press
Elthon D, Casey JF, Komor S (1982) Mineral chemistry of ultramafic cumulates from the North Arm Mountain massif of the Bay of Islands ophiolite: Evidence for high-pressure crystal fractionation of oceanic basalts. J Geophys Res 87:8717–8734
Elthon D, Ridley WI (1979) Comments on: “The partitioning of Ni between olivine and silicate melt”. Earth Planet Sci Lett 44:162–164
Fisk MR, Bence AE (1980) Experimental crystallization of chrome spinel in FAMOUS basalt 527-1-1. Earth Planet Sci Lett 48:111–123
Flower MFJ, Robinson PT (1979) Evolution of the FAMOUS ocean ridge segment: Evidence from submarine and deep-sea drilling investigations. In: Talwani M, Harrison CG, Hayes DE (eds) Deep Drilling Results in theAtlantic Ocean: Ocean Crust. Maurice Ewing Ser., vol. 2, pp 314–330 Am Geophys Union, Washington DC
Ford CE, Russell DG, Craven MR (1983) Olivine-liquid equilibria: Temperature, pressure and composition dependence of the crystal/liquid cation partition coefficients for Mg, Fe2+, Ca and Mn. J Petrol 24:256–265
Frey F, Suen CJ, Stockman HW (1985) The Ronda high temperature peridotite: Geochemistry and petrogenesis. Geochim Cosmochim Acta 49:2469–2492
Grove TL, Bence AE (1977) Experimental study of pyroxene-liquid interaction in quartz-normative basalt 15597. Proc Lunar Sci Conf 8th: 1549–1579
Grove TL, Bence AE (1979) Crystallization kinetics in a multiply saturated basalt magma: An experimental study of Luna 24 ferro-basalt. Proc Lunar Planet Sci Conf 10th: 429–478
Grove TL, Bryan WB (1983) Fractionation of pyroxene-phyric MORB at low pressure: An experimental study. Contrib Mineral Petrol 84:293–309
Hart SR, Davis KE (1978) Nickel partitioning between olivine and silicate melt. Earth Planet Sci Lett 40:203–219
Irving AJ (1978) A review of experimental studies of crystal/liquid trace element partitioning. Geochim Cosmochim Acta 42:743–770
Langmuir CH (1980) A major and trace element approach to basalts. Ph. D. thesis, State Univ of New York, Stony Brook
Langmuir CH, Weaver JS (1982) A general method of calculating phase equilibria applied to complex crystallization processes in oceanic basalts (abstract). EOS Trans Am Geophys Union 63:475
Langmuir CH, Bender JF, Bence AE, Hanson GN, Taylor SR (1977) Petrogenesis of basalts from the FAMOUS area: Mid-Atlantic Ridge. Earth Planet Sci Lett 36:133–156
Leeman WP (1974) Experimental determination of partitioning of divalent cations between olivine and basaltic liquid. Part II. Ph D thesis University of Oregon, Eugene, Oregon
le Roex AP, Erlank AJ, Needham HD (1981) Geochemical and mineralogical evidence for the occurrence of at least three distinct magma types in the “FAMOUS” region. Contrib Mineral Petrol 77:24–37
Longhi J, Walker D, Hays JF (1978) The distribution of Fe and Mg between olivine and lunar basaltic liquids. Geochim Cosmochim Acta 42:1545–1558
McIntire WL (1963) Trace element partition coefficients-a review of theory and application to geology. Geochim Cosmochim Acta 27:1209–1264
Morioka M (1981) Cation diffusion in olivine —II. Ni-Mg, Mn-Mg, Mg and Ca. Geochim Cosmochim Acta 45:1573–1580
Nabelek PI (1980) Nickel partitioning between olivine and liquid in natural basalts: Henry's Law behavior. Earth Planet Sci Lett 48:293–302
Nabelek PI, Langmuir CH, Bence AE (1981) The polybaric history of FAMOUS basalt 567-1-1: Evidence from trace elements in olivine. Microbeam Anal 151–154
Nisbet EG, Fowler CMR (1978) Mid-Atlantic Ridge at 37° and 45° N: some geophysical and petrological constraints. Geophys J R Astron Soc 54:631–660
Sato H (1977) Nickel content of basaltic magmas: identification of primary magmas and a measure of the degree of olivine fractionation. Lithos 10:113–120
Schilling J-G, Zajac M, Evans R, Johnston T, White W, Devine JC, Kingsley R (1983) Petrologic and geochemical variation along the Mid-Atlantic Ridge from 29° to 73° N. Am J Sci 283:510–586
Simkin T, Smith JV (1970) Minor element distribution in olivine. J Geol 78:304–325
Stakes DS, Shervais JW, Hopson CA (1984) The volcanic-tectonic cycle of the FAMOUS and AMAR valleys, Mid-Atlantic Ridge (36° 47′N): Evidence from basalt glass and phenocryst compositional variations for a steady state magma chamber beneath the valley midsection. AMAR 3. J Geophys Res 89:6995–7028
Roeder PK, Emslie RF (1970) Olivine-liquid gnequilibrium. Contrib Mineral Petrol 29:275–289
White WM, Bryan WB (1977) Sr-isotope, K, Rb, Cs, Sr, Ba and rare-earth geochemistry of basalts from the FAMOUS area. Geol Soc Am Bull 88:571–576
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Nabelek, P.I., Langmuir, C.H. The significance of unusual zoning in olivines from FAMOUS area basalt 527-1-1. Contr. Mineral. and Petrol. 93, 1–8 (1986). https://doi.org/10.1007/BF00963580
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DOI: https://doi.org/10.1007/BF00963580