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microtomes

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Journal Article
Published: 01 June 1983
Journal of Sedimentary Research (1983) 53 (2): 667–669.
Journal Article
Published: 01 April 1997
European Journal of Mineralogy (1997) 9 (2): 449–456.
Journal Article
Journal: GSA Bulletin
Published: 01 January 1972
GSA Bulletin (1972) 83 (1): 129–142.
... undistorted microtome sections (15μ thick) were cut from oriented samples of peat impregnated with paraffin. By comparison with reference slides of modern plant tissues, it was possible to identify the genera and sometimes the species of plants contributing to the peat even though there were only much-altered...
Journal Article
Published: 01 July 1969
Journal of Paleontology (1969) 43 (4): 1046–1048.
...Benjamin N. Akpati Abstract The use of biological microtomes in sectioning foraminiferal tests makes it possible to cut continuous serial sections from the same specimen for light microscopy and also offers a potential for use in cutting electron microscopy size sections. Epon 812 (mixture B) gives...
Image
( T Op row  ) Scanning electron microscope images of an anhydrous, chondrit...
Published: 01 June 2016
F igure 4 ( T Op row ) Scanning electron microscope images of an anhydrous, chondritic porous interplanetary dust particle (IDP) and a hydrated, chondritic smooth IDP. ( M iddle row ) Backscatter electron images of microtome sections of the same two particles where brightness is determined
Image
1–3 illustrate the encapsulation process.  1 A paper model on a thin film o...
Published: 01 January 2008
agarose block with the specimen at the center helps with location of the sample on the microtome. 4–9 illustrate preparation of the sample block for ultramicrotomy. 4 Guide lines for orientation are drawn with indelible ink. Note the central position of the blue agarose block in the polymerized resin
Image
F ig . 11. Chemical mapping of pseudo-cubic crystals of
      aluminum-phos...
Published: 01 May 2000
F ig . 11. Chemical mapping of pseudo-cubic crystals of aluminum-phosphate-sulfate solid-solution series from the Agua Shuca kaolin deposit using TEM-EDX and microtome sections (size: approximately 150 μm).
Image
TEM images on <span class="search-highlight">microtomed</span> samples. ( a ) Low-magnification image of poorly c...
Published: 01 November 2004
F igure 5. TEM images on microtomed samples. ( a ) Low-magnification image of poorly crystallized phyllomanganates encrusting Si fossils. ( b ) Poorly crystallized phyllomanganates on the edge of a diatom frustul remain ( c ). SAED on poorly crystallized phyllomanganates.
Image
F ig . 10. Chemical mapping of aluminum-phosphate-sulfate
      and aluminu...
Published: 01 May 2000
F ig . 10. Chemical mapping of aluminum-phosphate-sulfate and aluminum-sulfate mineral aggregates from the Agua Shuca kaolin deposit using TEM-EDX and microtome sections (size: approximately 150 μm). White arrow in Fe denotes jarosite overgrowth.
Image
( a ) TEM image of Paua shell  H. iris  showing the tile regularity compare...
Published: 01 November 2005
F igure 3. ( a ) TEM image of Paua shell H. iris showing the tile regularity compared to that of a silver P. maxima pearl shown in the TEM image ( b ). Figure ( b ) also shows microtome scour marks orientated approximately perpendicular to layers of tiles.
Journal Article
Published: 01 October 2017
American Mineralogist (2017) 102 (10): 2142–2145.
... of Cr in silicate minerals and glasses. Silicates are more soluble and generally more susceptible to weathering than the refractory mineral chromite, the principal ore mineral of Cr. Studies at the nanoscale using a combination of advanced sample preparation via microtoming and focused ion beam...
FIGURES
Image
F ig . 1. TEM image of a <span class="search-highlight">microtomed</span> slice of the white biofilm from the Piq...
Published: 01 September 2002
F ig . 1. TEM image of a microtomed slice of the white biofilm from the Piquette mine in southwestern Wisconsin. Round black aggregates are ZnS; note microbial cells on the right side of the image. Selected-area diffraction image of ZnS ball is shown at lower left.
Image
Localization of IR and ESEM mapping area on an ESEM image of the <span class="search-highlight">microtome</span> ...
Published: 01 November 2010
Fig 3. Localization of IR and ESEM mapping area on an ESEM image of the microtome section. Clinoptilolite tuff grains in lighter gray are surrounded by a matrix of portlandite, C–S–H, and C–A–H. M1–M8 circles indicate measurement positions of spectra displayed in Fig. 4 .
Journal Article
Published: 01 August 2014
Clays and Clay Minerals (2014) 62 (4): 336–353.
... examined. To prevent possible intrusion of epoxy resin into interlayers during embedding, the clay samples were first embedded in epoxy, sectioned with an ultra microtome, and then treated with octadecylammonium cations before examination using HRTEM. Lattice-fringe images showed that lower-charge...
FIGURES | View All (7)
Image
TEM images on <span class="search-highlight">microtomed</span> samples (71GC01 and 79GC01). ( a ) Mn-rich mineral...
Published: 01 November 2004
F igure 6. TEM images on microtomed samples (71GC01 and 79GC01). ( a ) Mn-rich mineralization showing a cellular structure. The view at high magnification displays filament-like structure formed by the aggregation of nano-particles. ( b ) Mn-rich nanoparticle mineralizations fossilizing cell
Journal Article
Published: 01 August 2003
Clays and Clay Minerals (2003) 51 (4): 382–389.
...-reduced and Fe(III)-reduced nontronite, observed by EC-TEM, exhibited fringes with mean d 001 spacings of 1.50 nm (standard deviation, σ = 0.08 nm) and 1.26 nm (σ = 0.10 nm), respectively. In comparison, the same samples embedded with Nanoplast resin, sectioned by microtome, and observed using...
FIGURES | View All (6)
Journal Article
Published: 01 June 1987
Journal of the Geological Society (1987) 144 (3): 423–434.
.... Botanical parent material, inferred from 13 C signatures and microtome sections, is always freshwater, originating either in forested swamps, or under herbaceous (floating) mats. Sphagnum spp. is essentially absent. In order for peat to accumulate, rates of accretion and subsidence must balance. Long-term...
Journal Article
Journal: GSA Bulletin
Published: 01 December 1973
GSA Bulletin (1973) 84 (12): 3867–3878.
... important peat producers throughout much of the history of peat formation in the swamp. The peat samples were dehydrated in alcohol, embedded in paraffin (using the methods of Cohen and Spackman, 1972), and sectioned (to 15 µ) with a sliding microtome. The microscopic features found to be most useful...
Journal Article
Journal: GSA Bulletin
Published: 01 August 1970
GSA Bulletin (1970) 81 (8): 2477–2482.
...ARTHUR D COHEN Abstract An allochthonous beach deposit of peat from southern Florida was investigated with the aid of oriented microtome sections. Because of its strong microlamination and lack of ingrown roots, this peat had a microscopic structure similar to that seen in thin sections...
Journal Article
Published: 01 January 1968
Micropaleontology (1968) 14 (1): 97–104.
... by maceration. Layering and ornamentation may be observed in surface views of detached megaspore membranes, but clarity is greater if microtome sections are prepared. Fragments of the nucellus which sometimes remain associated with the megaspore membranes supplement these features and aid in the recognition...