Electron microscopy of high-pressure phases synthesized from natural olivine in diamond anvil cell
- 117 Downloads
- 32 Citations
Abstract
The products of the transformation of natural (Mg0.83Fe0.17)2SiO4 olivine have been prepared at various high pressures (between 25 GPa and 90 GPa), and high temperature in a laser-heated diamond-anvil cell (DAC). Studies of the high-pressure phases have been made by transmission electron microscopy (TEM), and X-ray microanalysis.
The olivine/spinel boundaries exhibit all the characteristics of a diffusionless shear transition, having a finely sheared structure and a constant orientation relationship between the close-packed planes of the two structures ((100)ol∥(111)sp).
The TEM observations of zones where olivine (or spinel) transforms into post-spinel phases show that the transformation possesses the features of an eutectoïdal decomposition, leading to a lamellar intergrowth of magnesiowüstite (Mg,Fe)O and perovskite (Mg,Fe)SiO3. With increasing temperature and/or decreasing pressure, the grain size of the high-pressure phases increases and obeys an Arrhenius law with an activation volume equal to zero. (Mg,Fe)O grains exhibit a very high density of dislocations (higher than 1011cm−2), whereas (Mg,Fe)SiO3 grains exhibit no dislocations but systematic twinning. The composition plane of the twins is (112) of the GdFeO3-type perovskite, corresponding to the {110} plane of the cubic lattice of ideal perovskite.
Keywords
Olivine Perovskite Orientation Relationship Transmission Electron Microscopy Observation Shear TransitionPreview
Unable to display preview. Download preview PDF.
References
- Anderson DL (1977) Composition of the mantle and core. Ann Rev Earth Planet Sci 5:179–202Google Scholar
- Ashworth JR, Barber DJ (1977) Electron microscopy of some strong meteorites. Phil Trans R Soc London 286:493–506Google Scholar
- Bassett WA (1979) The diamond cell and the nature of the Earths mantle. Ann Rev Earth Planet Sci 7:357–384Google Scholar
- Boland JN, Liebermann RC (1983) Mechanism of the olivine to spinel phase transformation in Ni2SiO4. Geophys Res Lett 10:87–90Google Scholar
- Boland JN, Liu L (1983) Olivine to spinel transformation in Mg2SiO4 via faulted structures. Nature 303:233–235Google Scholar
- Carter NL, Raleigh CB, De Carli PS (1968) Deformation of olivine in stony meteorites. J Geophys Res 73:5439–5461Google Scholar
- Doukhan N, Doukhan JC (1986) Dislocations in perovskites BaTiO3 and CaTiO3. Phys Chem Minerals 13:403–410Google Scholar
- Ericsson T (1966) The temperature and contractions dependence of the stacking fault energy in the Co-Ni system. Acta Metall 14:853–865Google Scholar
- Fournelle RA, Clark JB (1972) The genesis of the cellular precipitation reaction. Metall Trans 3:2757–2767Google Scholar
- Furnish MD, Bassett A (1983) Investigation of the mechanism of the olivine-spinel transition in fayalite synchrotron radiation. J Geophys Res 88:10333–10341Google Scholar
- Guyot F, Madon M, Peyronneau J, Poirier JP (1988) X-ray microanalyses of high-pressure phases synthesized from natural olivine in diamond anvil cell. In preparationGoogle Scholar
- Heinz DL, Jeanloz R (1986) Temperature distribution in laserheated diamond-anvil cells. In “High pressure Research”. Applications in Geophysics and Geochemistryin Press. US-Japan Seminar. Program with Abstracts.Google Scholar
- Heinz DL, Jeanloz R (1987) Measurement of the melting curve of (Mg.9), Fe.1SiO3 at lower mantle conditions and its geophysical implications. J Geophys Res 92:11437–11444Google Scholar
- Ito E, Takahashi E, Matsui Y (1984) The mineralogy and chemistry of the lower mantle: an implication of the ultrahigh-pressure phase relations in the system MgO-FeO-SiO2. Earth Planet Sci Lett 67:238–248Google Scholar
- Jeanloz R, Thompson AB (1983) Phase transitions and mantle discontinuities. Rev Geophys Space Phys 21:51–74Google Scholar
- Lacam A, Madon M, Poirier JP (1980) Olivine glass and spinel formed in a laserheated diamond-anvil high-pressure cell. Nature 289:155–157Google Scholar
- Lauterjung J, Will G (1986) The kinetics of the olivine spinel transformation in Mg2GeO4 under high pressure and temperature. Physcia 139 and 140 B:343–346Google Scholar
- Liu L (1978) High pressure decomposition of Ca2GeO4 and Ca2MnO4 with the K2NiF4-type structures. Phys Earth Planet Inter 17:29–33Google Scholar
- Liu L (1979) Phase transformation and the constitution of the deep mantle. In “The earth: its origin, structure and evolution” ed. MW Mc Elhinny London, Academic Press, 177–202Google Scholar
- Livingston JD, Cahn JW (1974) Discontinuous coarsening of aligned eutectoïds. Acta Metall 22:495–503Google Scholar
- Madon M (1981) Can γ-spinel give garnet in the mantle transition zone? Terra Cognita SI, 89Google Scholar
- Madon M, (1986) Cellule à enclumes de diamant et microscopie electronique en transmission: Étude expérimentale des transformations de phase du manteau terrestre. These de Doctorat d'Etat, Université Paris 6, 298 ppGoogle Scholar
- Madon M, Poirier JP (1980) Dislocations in spinel and garnet high pressure polymorphs of olivine and pyroxene: Implications for mantle rheology. Science 207:66–68Google Scholar
- Madon M, Poirier JP (1983) Transmission electron microscope observations of α, β and γ-(Mg, Fe)2SiO4 in shocked meteorites: planar defects and polymorphic transitions. Phys Earth Planet Inter 33:31–44Google Scholar
- Madon M, Peyronneau J, Poirier JP (1984) Diamond anvil cell≅Shock wave gun? J Phys 45:117–120Google Scholar
- Madon M, Bell PM, Mao HK, Poirier JP (1980) Transmission electron diffraction and microscopy of synthetic high-pressure MgSiO3 phase with perovskite structure. Geophys Res Lett 7:629–632Google Scholar
- Mao HK (1972) Electrical and optical properties of the olivine series at high pressure. Carnegie Inst Washington Yearb 72:552–554Google Scholar
- Mao HK, Bell PM (1977) Static experiments to determine the volume equation of state of four metals (Cu, Mo, Pd and Ag) and calibration of the ruby R1 pressure scale. Carnegie Inst Washington Yearb 76:650–654Google Scholar
- Muller O, Roy R (1974) The major ternary structural families. Springer Verlag, Berlin Heidelberg New York, 487 ppGoogle Scholar
- Nakajima S, Hamaya N (1982) Olivine-spinel transformation mechanism in single crystal Ni2SiO4. EOS 63:431Google Scholar
- Nicolas A, Poirier JP (1976) Crystalline plasticity and solid state flow of metamorphic rocks. Wiley Interscience, London, 444 ppGoogle Scholar
- Peyronneau J, Madon M, Poirier JP (1984) Indirect pressure measurements in diamond cell up to 1 megabar. J Phys 45:403–404Google Scholar
- Poirier JP (1981a) Martensitic olivine-spinel transformation and plasticity of the mantle transition zone. In “Anelasticity in the Earth”. Am Geophys Union, 122 ppGoogle Scholar
- Poirier JP (1981b) On the kinetics of the olivine-spinel transition. Phys Earth Planet Inter 26:179–187Google Scholar
- Poirier JP, Peyronneau J, Madon M, Guyot F, Revcolevschi A (1986) Eutectoïd phase transformation of olivine and spinel into perovskite and rocksalt structures. Nature 321:603–605Google Scholar
- Price GD, Parker SC, Yeomans J (1985) The energetics of polytypic structures: a computer simulation of magnesium silicate spinelloïds. Acta Crystallogr 41:231–239Google Scholar
- Price GD, Putnis A, Agrell SO (1979) Electron petrography of shocked produced veins in the Tenham chondrite. Contrib Mineal Petrol 71:211–218Google Scholar
- Putnis A, Price GD (1979) High-pressure (Mg,Fe)2SiO4 phases in the Tenham chondrite meteorite. Nature 280:217–218Google Scholar
- Reid AF, Ringwood AE (1970) the crystal chemistry of dense M3O4 polymorphs: high-pressure Ca2GeO4 of K2NiF4 structure type. J Solid State Chem 1:557–565Google Scholar
- Rubie DC, Champness PE (1987) The evolution of microstructure during the transformation of Mg2GeO4 olivine to spinel. Bull Mineral 110:471–480Google Scholar
- Sasaki S, Prewitt CT, Liebermann RC (1983) The crystal structure of CaGeO3 perovskite and the crystal chemistry of the GdFeO3-type perovskites. Am Mineral 68:1189–1198Google Scholar
- Strudel JL (1983) Mechanical properties of multiphase alloys. In “Physical Metallurgy”. RW Cahn und P Haasen (ed) North Holland Physics publishing, 1411–1485Google Scholar
- Vaughan PJ, Kohlstedt DL (1981) Cation stacking faults in magnesium germanate spinel. Phys Chem Minerals 7:241–245Google Scholar
- Vaughan PJ, Green HW, Coe RS (1982) Is the olivine-spinel phase transformation martensitic? Nature 298:357–358Google Scholar
- Veyssiere P, Rabier J, Grilhe J (1975) Stacking fault energy computations in oxides with normal and inverse spinel structures. Phys Status Solidi 31:605–614Google Scholar
- Weidner DJ (1986) Mantle model base on measured physical properties of minerals. In “Chemistry and Physics of Terrrestrial Planets”. Advances in Physical Geochemistry, vol. 6, SpringerVerlag New-York, 251–274Google Scholar
- Yagi T, Mao HK, Bell PM (1978) Structure and crystal chemistry of perovskite-type MgSiO3. Phys Chem Minerals 3:97–110Google Scholar
- Yagi T, Mao HK Bell PM (1979) Phase relations in the system MgO-FeO-SiO2 between 150 and 700 kbar at 1000 °C. Carnegie Inst Washington Yearb 78:614–618Google Scholar
- Yagi T, Akaogi M, Shimomura O, Suzuki T, Akimoto S (1987) In situ observation of the olivine-spinel phase transformation in Fe2SiO4 using synchrotron radiation. J Geophys Res 92:6207–6213Google Scholar