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  • 1
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 403 (2000), S. 883-886 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The formation mechanism of terrestrial planetary cores is still poorly understood, and has been the subject of numerous experimental studies. Several mechanisms have been proposed by which metal—mainly iron with some nickel—could have been extracted from a silicate mantle to ...
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1420-9136
    Keywords: Key words: Simple shear deformation, structural geology, seismic anisotropy, partial melting, lattice preferred orientation, shear localization.
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract —A brief outline is given on experimental studies carried out in the Minnesota Mineral and Rock Physics Laboratory of microstructural evolution and rheology of mantle mineral aggregates or their analogues, using a simple shear deformation geometry. A simple shear deformation geometry allows us to unambiguously identify controlling factors of microstructural evolution and to obtain large strains at high pressures and temperatures, and thus provides a unique opportunity to investigate the "structural geology of the mantle." We have developed a simple shear deformation technique for use at high pressures and temperatures (pressure up to 16 GPa and temperature up to 2000 K) in both gas-medium and solid-medium apparati. This technique has been applied to the following mineral systems (i) olivine aggregates, (ii) olivine basaltic melt, (iii) CaTiO3 perovskite aggregates. The results have provided important data with which to understand the dynamics of the earth’s mantle, including the geometry of mantle convection, mechanisms of melt distribution and migration beneath mid-ocean ridges, and the mechanisms of shear localization. Limitations of laboratory studies and future directions are also discussed.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 95 (1987), S. 226-230 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract A suite of heat-treatment experiments have been performed to test the high-temperature stability of San Carlos olivine within the theoretical $${\text{p}}_{{\text{O}}_{\text{2}} } $$ stability field at one atmosphere total pressure. Exsolution or contamination products did not form on the surfaces of samples which were surrounded by olivine, magnesia, or alumina. In contrast, silica-rich phases developed on the surfaces of samples which were in line-of-sight contact with silica or platinum. These silica-rich phases result from interaction of the olivine with silica or platinum in the furnace environment via vapor phase transport or surface diffusion, rather than from diffusion of excess silica from the bulk to the surface as suggested by Jaoul et al. (1984, 1985). This conclusion is consistent with the reported slow rate of diffusion of silicon in olivine and with the lack of internal precipitation of silica-rich phases. Consequently, it is concluded that San Carlos olivine does not contain silica in excess of the solubility limit under conditions which are within the $${\text{p}}_{{\text{O}}_{\text{2}} } $$ -T stability field for this (Mg,Fe,Ni)-olivine.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 11 (1984), S. 5-16 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract The sintering behavior of olivine and olivine-basalt aggregates has been examined at temperatures near 1,300° C. Experimental factors contributing to rapid sintering kinetics and high-density, fine-grained specimens include: (i) the uniform dispersion of basalt throughout the specimen, (ii) a very fine, uniform particle size for the olivine powder, (iii) oxygen fugacities near the high P O2 end of the olivine stability field, and (iv) rapid heating to the sintering temperature. Olivine-basalt specimens prepared from olivine particles coated with a synthetic basalt achieve chemical and microstructural equilibrium more rapidly, as well as produce higher density and finer grain-sized aggregates, than do specimens prepared by mechanical mixing of olivine and natural basalt powders. The grain boundary mobility for olivine, measured for olivine-basalt aggregates which have undergone secondary recrystallization, is on the order of 2×10−15 (m/s)/(N/m2) in the temperature range 1,300–1,400° C. Solution-precipitation (pressure-solution) processes make an important contribution to the development of the microstructure in olivine-basalt aggregates.
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 13 (1986), S. 351-356 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract Creep experiments have been performed on samples from a single crystal of vanadium-doped forsterite under controlled $$p_{{\text{O}}_2 } $$ conditions to investigate the effects of the addition of substitutional defects in the tetrahedral lattice sites. The addition of vanadium causes marked changes in the flow behavior of the forsterite, with a net increase in the creep rate at high $$p_{{\text{O}}_2 } $$ and a new $$p_{{\text{O}}_2 } $$ -dependent flow regime at low $$p_{{\text{O}}_2 } $$ conditions. These observations can be interpreted as resulting from changes in the majority defect species that maintain the charge neutrality within the crystal. A climb-controlled dislocation creep model for the high-temperature deformation of vanadium-doped forsterite is proposed in which either (i) movement of uncharged jogs is rate-limited by the diffusion of silicon via a vacancy mechanism or (ii) movement of positively charged jogs is rate-limited by diffusion of oxygen via a vacancy mechanism.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 22 (1995), S. 489-503 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract To investigate the point defect chemistry and the kinetic properties of manganese olivine Mn2SiO4, electrical conductivity (’) of single crystals was measured along either the [100] or the [010] direction. The experiments were carried out at temperatures T=850–1200 °C and oxygen fugacities $$f_{{\text{O}}_{\text{2}} } = 10^{ - 11} - 10^2 $$ atm under both Mn oxide (MO) buffered and MnSiO3 (MS) buffered conditions. Under the same thermodynamic conditions, charge transport along [100] is 2.5–3.0 times faster than along [010]. At high oxygen fugacities, the electrical conductivity of samples buffered against MS is ∼1.6 times larger than that of samples buffered against MO; while at low oxygen fugacities, the electrical conductivity is nearly identical for the two buffer cases. The dependencies of electrical conductivity on oxygen fugacity and temperature are essentially the same for conduction along the [100] and [010] directions, as well as for samples coexisting with a solid-state buffer of either MO or MS. Hence, it is proposed that the same conduction mechanisms operate for samples of either orientation in contact with either solid-state buffer. The electrical conductivity data lie on concave upward curves on a log-log plot of σ vs $$f_{{\text{O}}_{\text{2}} } $$ , giving rise to two $$f_{{\text{O}}_{\text{2}} } = 10^{ - 11} - 10^2 $$ regimes with different oxygen fugacity exponents. In the low- $$f_{{\text{O}}_{\text{2}} } = 10^{ - 11} - 10^2 $$ regime $$\left( {f_{{\text{O}}_{\text{2}} } 〈 10^{ - 7} {\text{atm}}} \right)$$ , the $$f_{{\text{O}}_{\text{2}} } = 10^{ - 11} - 10^2 $$ exponent, m, is 0, the MnSiO3-activity exponent, q, is ∼0, and the activation energy, Q, is 45 kJ/mol. In the high $$f_{{\text{O}}_{\text{2}} } = 10^{ - 11} - 10^2 $$ regime $$\left( {f_{{\text{O}}_{\text{2}} } 〉 10^{ - 7} {\text{atm}}} \right)$$ , m=1/6, q=1/4–1/3, and Q=45 and 200 kJ/mol for T〈1100 °C and T〉1100 °C, respectively. Based on a comparison of experimental data with results from point defect chemistry calculations, it is proposed that the change in m with $$f_{{\text{O}}_{\text{2}} } = 10^{ - 11} - 10^2 $$ is induced by a switch in charge neutrality condition. At low $$f_{{\text{O}}_{\text{2}} } = 10^{ - 11} - 10^2 $$ s, the charge neutrality condition is [e′]=[Mn Mn { ]; the hopping motion of electron holes h . is the dominant conduction mechanism. At high $$f_{{\text{O}}_{\text{2}} } = 10^{ - 11} - 10^2 $$ s, the charge neutrality condition is 2[V Mn · ]=[Mn Mn · ]; the hopping motion of electron holes h . and the migration of Mn ions associated with a counter flow of divalent Mn vacancies V Mn · control electrical conduction at T〈1100 °C and T〉1100 °C, respectively.
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 7 (1981), S. 110-116 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract The effect of electron irradiation on defects in natural quartz grains has been studied using strong-beam and weak-beam transmission electron microscopy (TEM) techniques. Damage is visible soon after the sample is exposed to the electron beam. The defect centers grow with increased irradiation, but the density of centers is independent of electron dose. Dislocation images also widen during irradiation; the rate of widening is independent of Burgers vector and dislocation nodes widen without constriction. Both of these observations indicate that the widening of dislocation images is related to vitrification of the material in the vicinity of the dislocations rather than irradiation-assisted separation of partial dislocations. This interpretation is supported by observations on grain boundaries.
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 7 (1981), S. 241-245 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract Widely extended, cation stacking faults in experimentally deformed Mg2GeO4 spinel have been studied using transmission electron microscopy (TEM). The faults lie on {110} planes. The displacement vector is of the form $$\frac{1}{4}\left\langle {1\bar 10} \right\rangle $$ and is normal to the fault plane. The partial dislocations which bound the stacking fault have colinear Burgers vectors of the form $$\frac{1}{4}\left\langle {1\bar 10} \right\rangle $$ which are normal to the fault plane.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 9 (1983), S. 133-138 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract Electron diffraction and imaging techniques have been used to examine the structure and thickness of low-angle grain boundaries in olivine. For edge-on grain boundaries, a periodic array of dislocations in a boundary gives rise to sets of periodic rods of diffracted intensity that are recorded as streaks in the diffraction pattern. The length of these streaks provides a measure of the structural width of a boundary. For olivine, the structural width of a boundary with a given dislocation spacing is three to four times smaller than that in metals where the boundary width is approximately equal to the spacing between dislocations in the boundary.
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 18 (1991), S. 26-36 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract The wetting angle between silicate melts containing Ca, Li, Na, or K and olivine single crystals have been measured as part of an investigation of the dependence of the solid-liquid interfacial energy on melt composition and olivine orientation. The wetting angle increases with increasing silica content of the melt on (100) surfaces, but decreases with increasing silica content on (010) and (001) surfaces. For a given silica content, the wetting angle on (100) decreases in going from Ca to Li to Na to K, while the wetting angle on (010) and (001) increases in going from Ca to K-bearing melts. Based on published values for liquid-vapor interfacial energies, the observed changes in wetting angle with changes in melt composition indicate that the solid-liquid interfacial energy increases with increasing silica content of the melt for the (100) surface. However, for (010) and (001) surfaces, the variation of the solid-liquid interfacial energy with silica content depends upon whether Ca or K is present in the melt. In addition, the solid-liquid interfacial energy depends upon the orientation of the olivine in the following manner: γ sl (010) ⩽γ sl (001) 〈γ sl (100) .
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