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  • 1
    Electronic Resource
    Electronic Resource
    [S.l.] : International Union of Crystallography (IUCr)
    Acta crystallographica 52 (1996), S. 850-878 
    ISSN: 1600-5724
    Source: Crystallography Journals Online : IUCR Backfile Archive 1948-2001
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: The geometry of the reciprocal space of cylindrically and conically rolled microstructures is described. The simpler cylindrical case is first discussed, followed by the conical case; in both cases, the observations and then the theory are described. The theory is compared with observations on chrysotiles, the structural and microstructural features of which are briefly recalled. The reciprocal space of an infinite 3D crystal consists of a lattice of discrete nodes. If a crystalline sheet is curled up into a cylindrical scroll (or into concentric cylinders), the corresponding reciprocal space is obtained by rotating this set of lattice points about a line parallel to the cylinder axis through the origin of reciprocal space. The lattice nodes thereby describe geometrical loci that, in this simple case, are circles in planes perpendicular to the rotation axis. For a general orientation of the rotation axis, each node produces its own circle. This is the case when the fibre has chiral character. For certain symmetrical orientations of the axis, `degeneracy' occurs and two (or more) nodes may lead to the same circular locus. This is the case for achiral fibres. The curvature often causes disorder in the stacking of successive cylindrical sheets – this leads to `coronae' instead of sharp circles – especially in the concentric cylinder case. In the diffraction pattern, these produce spots that are streaked in the sense away from the axis. In ideal cylindrical scrolls, the structures in successive layers, as viewed along a radial line c, are shifted relative to each other over 2π times the layer thickness; this may lead to superperiods along the normal c to the sheet planes if this shift is commensurate with the lattice vectors in the sheet plane, i.e. with its translation symmetry. The superperiod is clearly related to the sheet thickness, which may be more than one bilayer. If the crystalline sheet is curled up into a cone, the reciprocal-space loci become curves that are situated on spheres of constant spatial frequency, called spherical spirals instead of the circles in the cylindrical case. Each reciprocal-lattice node describes such a spiral traced out by a node point subject to the coupled rotations about the cone axis and about the local normal to the cone surface. The equations of such spirals are derived and their symmetry properties are studied analytically. The spiral's shape is a function of the semi-apex angle of the cone. For an arbitrary cone angle, these curves are not closed; they completely fill a band on the surface of the sphere. For certain discrete cone angles, which turn out to be essentially determined by the condition of good epitaxic fit between successive sheets of the cone, the spherical spirals become closed curves. The conditions under which several node points, belonging to the same spatial frequency, trace out the same spherical spiral are discussed: i.e. the conditions for degeneracy are formulated. The point symmetries of the sets of spherical spirals belonging to the same spatial frequency are found to depend on characteristic values of the semi-apex angle. All turns of a conical scroll are in fact formed from a single sheet. The structure in any given turn is rotated relative to that in the adjacent turn over a constant angle, only determined by the semi-apex angle. If this rotation angle is commensurate with 2π, superperiods can be formed, visible as reinforcements in streaks that are parallel to the generators of the cone formed by the set of normals to the conical surface. Also, this superperiod depends on the thickness of the sheet as well as on its rotation symmetry. Diffuse scattering is found to be concentrated on a V-shaped hyperboloid-like surface, the point of the V being situated on a spherical spiral. The intersection of this surface with the Ewald plane leads to V-shaped streaks attached by their apexes to the spots. They are the homologues of the simple streaks in the cylindrical case. Under certain conditions of beam incidence, the intersection is a hyperbole branch. Spot positions have been computed for a few characteristic diffraction conditions; they are found to represent adequately the observed spot patterns. A Mercator-like projection method is proposed to represent the spherical spirals in a plane and to construct geometrically the intersections with the Ewald plane for different angles of incidence. Throughout the paper, the analogies and the differences between the diffraction features of cylindrical and conical scrolls are emphasized and illustrated by observations on chrysotile.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Physics and chemistry of minerals 21 (1994), S. 330-343 
    ISSN: 1432-2021
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences , Physics
    Notes: Abstract Based on coexisting rolled chrysotile and polygonal serpentine fibers with 15 or 30 sectors each, a crystallographic model for polygonization of chrysotile is proposed. It is based on an assumed chrysotile-to-lizardite transition. Polygonization of chrysotile requires more likely 15 partial dislocations per turn, as required by polytype translational operators for serpentines. The observed number of sectors corresponds to the two most elastically stable arrays of dislocations. Homogeneous shear of the layer stacking arising from intersector kinking results in a cyclic distribution of twins and/or different polytypes. This makes the fiber axis a fivefold symmetry axis and consequently polygonal serpentine and chrysotile to be both forms of serpentine with local fivefold symmetry. This model is alternative to the recent crystallograpic model by Chisholm (1991, 1992).
    Type of Medium: Electronic Resource
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  • 3
    Publication Date: 2001-11-20
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
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  • 4
    Publication Date: 2015-05-13
    Description: This study investigates the oxidation of fayalite Fe 2 2+ SiO 4 that is present in lithophysae from a rhyolite flow (Obsidian Cliffs, Oregon). Textural, chemical, and structural analyses of the successive oxidation zones are used to constrain: (1) the oxidation processes of olivine, and (2) the role of temperature, chemical diffusion, and meteoric infiltration. Petrologic analyses and thermodynamic modeling show that the rhyolite flow emplaced at 800–950 °C. Fayalite-bearing lithophysae formed only in the core of the lava flow. Variations in the gas composition inside the lithophysae induced the oxidation of fayalite to a laihunite-1 M zone Fe 1 2+ Fe 2 3+ 1 (SiO 4 ) 2 . This zone is made of nano-lamellae of amorphous silica SiO 2 and laihunite-3 M Fe 2+ 1.6 Fe 3+ 1.6 0.8 (SiO 4 ) 2 + hematite Fe 2 O 3 . It probably formed by a nucleation and growth process in the fayalite fractures and defects and at fayalite crystal edges. The laihunite-1 M zone then oxidized into an "oxyfayalite" zone with the composition Fe 2+ 0.52 Fe 3+ 2.32 1.16 (SiO 4 ) 2 . This second oxidation zone is made of lamellae of amorphous silica SiO 2 and hematite Fe 2 O 3 , with a possible small amount of ferrosilite Fe 2+ SiO 3 . A third and outer zone, composed exclusively of hematite, is also present. The successive oxidation zones suggest that there may be a mineral in the olivine group with higher Fe 3+ content than laihunite-1 M . The transformation of laihunite-1 M to this "oxyfayalite" phase could occur by a reaction such as \[ 0.24{{\hbox{ Fe }}_{\hbox{ M }1}^{2+}}^{\hbox{ laihunite- }1M}+0.06{\hbox{ O }}_{2}=0.16\hspace{0.17em}{{\hbox{ Fe }}_{\hbox{ M }1}^{3+}}^{``\hbox{ oxyfayalite }''}+0.08{\square }^{``\hbox{ oxyfayalite }''}+0.04\hspace{0.17em}{\hbox{ Fe }}_{2}^{3+}{{\hbox{ O }}_{3}}^{\hbox{ hematite }} \] This would imply that Fe 3+ can also be incorporated in the M1 site of olivine.
    Print ISSN: 0003-004X
    Electronic ISSN: 1945-3027
    Topics: Geosciences
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  • 5
    Publication Date: 2017-07-28
    Description: The purpose of this work is to investigate the crystal growth parameters necessary or sufficient to obtain a crystal specifically of gem quality. We assume adequate chemistry is available. First, nucleation must occur with only a limited number of nuclei, otherwise too many crystals will be produced, and they will be too small to be faceted into a gem. Two growth mechanisms are readily documented for gems: Most commonly there is slow growth, driven by a spiral growth mechanism, leading to large single individuals. There are only a few examples of fast growth leading to gem-quality edifices: examples include "gota de aceite" Colombian emerald or the dendritic "pseudo cube" for gem diamonds. We have not documented the intermediate conditions between these two extremes in the Sunagawa diagram, which would correspond to 2D nucleation growth. The presence of inclusions is to be limited to desirable ones. Thus, in general, a good stability of the growth interface is the best guarantee of good clarity in the final gem. As for the interface, in general, growth conditions must be relatively stable over the period necessary to achieve growth. Perhaps surprisingly, it has become well documented that gem-quality near-colorless diamonds may have experienced quite a complex growth history. Therefore, the term stability has to be re-defined for each system producing a given gem. The length of time it takes to achieve crystallization of the gem has rarely been studied or estimated. Scientific evidence from experimental petrology and the growth of synthetic gems indicates that it does not take millions of years to grow a gem, but that this exercise may be achieved in a week to, arguably, a few years at the most. Available free space to grow does not appear always necessary, but it helps. Otherwise deformation, inclusions, and other negative effects may occur. Finally, no dramatic post-growth events, such as fracturing or etching, should affect the gem crystal.
    Print ISSN: 0008-4476
    Topics: Geosciences
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  • 6
    Publication Date: 2013-05-11
    Description: This work reports on the thermal decomposition of muscovite within a granite powder doped with 8.5 wt% ZnO and heated during 10 min to 68 h at 1175 °C, and the implications for the sequestration of Zn, and other heavy metalts in such decomposition products. Samples were characterized using analytical scanning and transmission electron microscopy. After 10 min, muscovite is completely pseudomorphosed by Si-rich glass, spinel structure phases, and minor mullite. Spinel phases incorporate Zn, but their compositions depend on their position within the muscovite pseudomorphs. Al-rich oxides crystallize at the core of the pseudomorphs while Zn-Al spinels are located at the rims. The most Al-rich spinels have compositions close to -Al 2 O 3 , a metastable transition alumina, with up to 5 wt% MgO, 2 wt% Fe 2 O 3 , 4 wt% ZnO, and 9 wt% SiO 2 . The most Zn-rich spinels show compositions intermediate between Al 2 O 3 and gahnite (ZnAl 2 O 4 ), with up to 31 wt% ZnO and significant contents of MgO (3 wt%), Fe 2 O 3 (5 wt%), and SiO 2 (10 wt%). After 68 h, stable spinels are gahnite close to the end-member composition with MgO and Fe 2 O 3 contents below ca. 5 wt%, and SiO 2 contents ca. 1 wt%. These results support the existence of a metastable solid solution between -Al 2 O 3 and gahnite. This experimental work shows that Zn can be incorporated in spinel structures after heating at 1175 °C during short durations and Zn is preferentially incorporated in the muscovite pseudomorphs as opposed to the Qtz-Fds glass. Consequently, the thermal breakdown of phyllosilicates can be a viable process to immobilize heavy metals such as Zn.
    Print ISSN: 0003-004X
    Electronic ISSN: 1945-3027
    Topics: Geosciences
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  • 7
    Publication Date: 2019
    Description: 〈span〉Lasnierite, (Ca,Sr)(Mg,Fe)〈sub〉2〈/sub〉Al(PO〈sub〉4〈/sub〉)〈sub〉3〈/sub〉, is a new phosphate mineral from Mt. Ibity, close to Itremo, central Madagascar. The mineral was found as inclusions accompanying blue lazulite and many other minerals in blue metaquartzite occasionally used as a gemstone or ornamental stone. The crystals were very small and embedded in quartz so that they could not be extracted mechanically, precluding any “classical” X-ray diffraction on either single-crystal or powder sample. Hence, Focused Ion Beam (FIB) lamellae were extracted and the structure was successfully solved and refined using the recently proposed method of precession electron diffraction tomography (PEDT) associated to dynamical refinement. This underlines the efficiency of this new method for defining mineral species on volumes too small to be manipulated by classical means of X-ray diffraction. Accompanying minerals include various phosphates, sulfates, oxides and silicates. Lasnierite occurs as transparent, near-colourless bladed crystals up to 120 × 60 μm in section. Only five crystals have been identified yet in our samples. The empirical formula, based on wavelength dispersive spectrometry (WDS) electron microprobe analyses and calculated on 12 (O+F) atoms per formula unit, is (Ca〈sub〉0.59〈/sub〉Sr〈sub〉0.37〈/sub〉)〈sub〉∑0.96〈/sub〉(Mg〈sub〉1.42〈/sub〉Fe〈sub〉0.54〈/sub〉)〈sub〉∑1.96〈/sub〉Al〈sub〉0.87〈/sub〉(P〈sub〉2.99〈/sub〉Si〈sub〉0.01〈/sub〉)〈sub〉∑3.00〈/sub〉(O〈sub〉11.41〈/sub〉F〈sub〉0.59〈/sub〉)〈sub〉∑12〈/sub〉. LA-ICPMS shows that concentrations of Li, Be and B are below the detection limit. The calculated density based on the empirical formula is 3.162 g cm〈sup〉−3〈/sup〉. Lasnierite is orthorhombic, space group 〈span〉Pbcn〈/span〉, with unit-cell parameters: 〈span〉a〈/span〉 = 6.2771(3) Å, 〈span〉b〈/span〉 = 17.684(3) Å, 〈span〉c〈/span〉 = 8.1631(4) Å, 〈span〉Z〈/span〉 = 4 and 〈span〉V〈/span〉 = 906.1(2) Å〈sup〉3〈/sup〉. The structure is new. The Raman spectra show characteristic peaks at 〈span〉99〈/span〉, 〈span〉122〈/span〉, 278, 〈span〉418〈/span〉, 510, 569, 590, 621, 661, 〈span〉985〈/span〉, 〈span〉1028〈/span〉, 〈span〉1040〈/span〉, 1063, 1100, 1126 and 1148 cm〈sup〉−1〈/sup〉 (most intense bands are italicised). Raman spectra also show the absence of H〈sub〉2〈/sub〉O and CO〈sub〉2〈/sub〉.〈/span〉
    Print ISSN: 0935-1221
    Electronic ISSN: 1617-4011
    Topics: Geosciences
    Published by Schweizerbart
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  • 8
  • 9
    Publication Date: 2016-09-09
    Print ISSN: 0004-637X
    Electronic ISSN: 1538-4357
    Topics: Physics
    Published by Institute of Physics
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  • 10
    Publication Date: 2011-06-01
    Print ISSN: 0016-7037
    Electronic ISSN: 1872-9533
    Topics: Chemistry and Pharmacology , Geosciences
    Published by Elsevier
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