Advances in Applying Electron Microscopy in Studying the Microstructure of Minerals

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Crystallography and Physical Chemistry of Minerals & Nanominerals".

Deadline for manuscript submissions: closed (15 September 2020) | Viewed by 6751

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Dipartimento di Scienze dell'Ambiente e della Terra, University of Milano - Bicocca, Milan, Italy

Special Issue Information

Dear Colleagues,

Transmission electron microscopy (TEM) is a comprehensive technique for the characterization of solid-state materials: With a single instrument, morphological features, microstructural information, crystallographic data, and chemical composition can be obtained. Since its first appearance in Mineral Sciences, TEM has represented an affective technique for the characterization of defects and their quantitative assessment in terrestrial and nonterrestrial materials (e.g., Phakey et al. 1972; Lally et al. 1976; Kitamura et al. 1987). Mineral deformation and transformation mechanisms in natural systems and experimental apparatuses would never have reached the current level of understanding without direct imaging and crystallographic analysis with TEM (e.g., Doukhan et al. 1985; Green 1993; Nord 1993), and large angle convergent beam electron diffraction (LACBED) has allowed the study of ideal and defective crystal structures at a finer level and even in beam sensitive materials (e.g., Cordier et al. 1995). As soon as resolution attained the unit cell scale, high-resolution electron microscopy (HRTEM) imaging provided details of atomic scale reactions, intergrowths, growing mechanisms, and the modularity of minerals (e.g., Buseck and Iijima 1974; van Landuyt & Amelinckx 1975; Kogure 2002). Our understanding of biopyriboles and concepts like polytypism and polysomatism would never have reached its contemporary level without the provision of the direct imaging of such phenomena by HRTEM (e.g., Chank and Liebau 1980; Veblen 1991; Baronnet 1993). The latest developments in electron microscopy allow the structure solution of nanosized materials, which was once hampered by the secular problem of dynamical scattering, through precession-assisted electron tomography (PEDT) (e.g., Mugnaioli 2009 and reference therein) and modern high angular annular dark field (HAADF) scanning transmission electron microscopy (STEM) techniques, and also allow the atomic scale imaging of beam sensitive materials, once hardly achievable with conventional HRTEM techniques, with the additional benefit of straightforwardly interpretable structures (e.g., Ciobanu et al. 2016 and reference therein). The present Special Issue aims to collect review papers and original research papers based on transmission electron microscopy techniques, with a special emphasis on those techniques that push their investigative limit down to the atomic scale.

References:

Baronnet A. (1993) Polytypism and stacking disorder. In: Mineral and reactions at the atomic scale: Transmission electron microscopy (P.R. Buseck Editor). Reviews in Mineralogy, 27, 231-282. Mineralogical Society of America, Washington, D.C.

Buseck P.R. & Iijima S. (1974) High resolution electron microscopy of silicates. Amer. Mineral., 59, 1-21.

Ciobanu C.L., Cook N.J., Maunders C., Wade B.P., Ehrig K. (2016) Focused ion beam and advanced electron microscopy for minerals: Insights and outlook from bismuth sulphosalts. Minerals, 6, 112.

Cordier  P., Morniroli  J. P. & Cherns D. (1995) Characterization of crystal defects in quartz by large-angle convergent-beam electron diffraction. Philosophical Magazine A, 72, 1421-1430.

Czank M. & Liebau F. (1980) Periodicity faults in chain silicates: A new type of planar lattice fault observed with high resolution electron microscopy. Phys. Chem. Minerals, 6, 85-93.

Doukhan J.C., Doukhan N., Kock P.S., Christie J.M. (1985) Transmission electron microscopy investigation of lattice defects in Al2SiO5 polymorphs and plasticity induced polymorphic transformations. Bull. Mineral., 108, 81-96.

Green H.W., 2nd (1993) Analysis of deformation in geological materials. In: Mineral and reactions at the atomic scale: Transmission electron microscopy (P.R. Buseck Editor). Reviews in Mineralogy, 27, 425-454. Mineralogical Society of America, Washington, D.C.

Kitamura M., Kondoh S., Morimoto N., Rossman G.R. & Putnis A. (1987) Planar OH-bearing defects in mantle olivine. Nature, 328, 143-145.

Kogure T. (2002) Investigations of micas using advanced transmission electron microscopy. In: Micas: Crystal Chemistry and Metamorphic Petrology (A. Mottana, F.P. Sassi, J.B. Thompson Jr. and S. Guggenheim, editors). Reviews in Mineralogy and Geochemistry, 46, 281-312. Mineralogical Society of America, Washington, D.C.

Lally J.S., Christie J.M., Nord, G.L. & Heuer A.H. (1976) Deformation, recovery and recrystallisation of lunar dunite 72417. Proc. Lunar Sci. Conf. 7th, 1845-1863.

Mugnaioli E., Gorelik T., and Kolb U. (2009) “Ab initio” structure solution from electron diffraction data obtained by a combination of automated diffrac­tion tomography and precession technique. Ultramicroscopy, 109, 758-765.

Nord G.L. (1993) Imaging transformation-induced microstructures. In: Mineral and reactions at the atomic scale: Transmission electron microscopy (P.R. Buseck Editor). Reviews in Mineralogy, 27, 455-508. Mineralogical Society of America, Washington, D.C.

Phakey P., Dollinger, G. & Christie J.M. (1972) Transmission electron microscopy of experimentally deformed olivine crystals. Geophys. Monogr., 16, 117-138.

van Landuyt J. & Amelinckx S. (1975) Multiple beam direct lattice imaging of new mixed-layer compounds of the bastnäsite-synchysite series. Amer. Mineral., 60, 351–358.

Veblen D.R. & Buseck, P.R. (1979) Chain width order and disorder in biopyriboles. Amer. Mineral., 64, 687-700.

Veblen D.R. (1991) Polysomatism and polysomatic series: A review and applications. Amer. Mineral., 76, 801-826.

Veblen D.R. (1993) Electron microscopy applied to nonstoichiometry, polysomatism, and replacement reactions in minerals. In: Mineral and reactions at the atomic scale: Transmission electron microscopy (P.R. Buseck Editor). Reviews in Mineralogy, 27, 181-229. Mineralogical Society of America, Washington, D.C.

Prof. Dr. GIANCARLO CAPITANI
Guest Editor

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Keywords

  • HRTEM
  • HAADF–STEM
  • LACBED
  • PEDT
  • polysomatism
  • polytypism

Published Papers (2 papers)

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Research

11 pages, 2315 KiB  
Communication
STEM-EELS Investigation of Planar Defects in Olivine in the Allende Meteorite
by Maya Marinova, Hugues Leroux, Priscille Cuvillier, Alexandre Gloter and Damien Jacob
Minerals 2021, 11(1), 35; https://doi.org/10.3390/min11010035 - 30 Dec 2020
Cited by 5 | Viewed by 2752
Abstract
The present study focuses on a detailed structural investigation at atomic scale of the planar defects that appear in the olivine grains in the Allende meteorite, and it aims to clarify their nature and the related formation mechanism. The investigation was performed using [...] Read more.
The present study focuses on a detailed structural investigation at atomic scale of the planar defects that appear in the olivine grains in the Allende meteorite, and it aims to clarify their nature and the related formation mechanism. The investigation was performed using advanced spectro-microscopy techniques such as atomically resolved high-angle annular dark field (HAADF) images coupled with electron energy loss spectroscopy in the scanning transmission electron microscopy mode (STEM-EELS). Two prominent structural features appear in the investigated olivine grains: (i) Exsolution platelets with a thickness between 2 and 10 nm with the spinel structure and chemical composition expressed as a solid solution between magnetite, chromite, and MgAl2O4. (ii) Thinner planar defects appeared with thickness between 2 to 4 atomic planes, which were rich in Fe and had a strong Fe3+ contribution. The structure of these defects was described by the crystalline lattice of the olivine grains with small distortion of the measured cationic distances, which can be related to Fe3+-Si substitution in the tetrahedral sites. Those metastable defects should have preceded the formation of the thicker spinel exsolutions and could have formed during an oxidizing event in the Allende parent body. Full article
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19 pages, 8190 KiB  
Article
Synchysite-(Ce) from Cinquevalli (Trento, Italy): Stacking Disorder and the Polytypism of (Ca,REE)-Fluorcarbonates
by Giancarlo Capitani
Minerals 2020, 10(1), 77; https://doi.org/10.3390/min10010077 - 18 Jan 2020
Cited by 11 | Viewed by 3513
Abstract
Synchysite-(Ce) at Cinquevalli occurs as fine needles intergrown with quartz in quartz-dikes and in association with altered K-feldspar and oxidized chalcopyrite as major constituents. Synchysite-(Ce) [Ca1.00(Ce0.43La0.26Nd0.17Y0.07Pr0.04Sm0.02Gd0.01)Σ=1.00 [...] Read more.
Synchysite-(Ce) at Cinquevalli occurs as fine needles intergrown with quartz in quartz-dikes and in association with altered K-feldspar and oxidized chalcopyrite as major constituents. Synchysite-(Ce) [Ca1.00(Ce0.43La0.26Nd0.17Y0.07Pr0.04Sm0.02Gd0.01)Σ=1.00(CO3)2(F0.58(OH)0.42)], shows an overgrowth rim of bastnäsite-(Ce) [(Ce0.34La0.25Nd0.17Pb0.07C a0.06Y0.06Pr0.04S m0.02Gd0.01)Σ=1.00C O3(F0.75(OH)0.25)]. Unit cell refinement of synchysite (C2/c) and bastnäsite (P62c) led to a = 12.272(4), b = 7.100(2), c = 18.640(5) Å, β = 102.71(5)°, and a = 7.085(1), c = 9.746(2) Å, respectively. Polysomatic faults are sporadic, but polytypic disorder is widespread. High resolution transmission electron microscopy images taken along [100] or ⟨130⟩ show an apparent order and the related diffraction patterns are streak-free. Conversely, along [010] or ⟨110⟩, a high density of stacking faults is observed and the related diffraction patterns show hhl rows with h ≠ 3n affected by streaks. No ordered domain larger than a few unit cells was detected. The stacking sequence of (Ca,REE)-fluorcarbonates can be compared with subfamily-B mica polytypes (2M2, 2O and 6H), which are characterized by n·60° (n = odd) rotations. Subfamily-A polytypes (1M, 2M1 and 3T), characterized by n·60° (n = even) rotations, should not be possible. Synchysite, characterized by ±60° rotations, can be likened to the 2M2 polytype. Full article
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