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carbonitrides

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Journal Article
Published: 01 August 2017
American Mineralogist (2017) 102 (8): 1667–1676.
...Felix Kaminsky; Richard Wirth Abstract The first finds of iron nitrides and carbonitride as inclusions in lower-mantle diamond from Rio Soriso, Brazil, are herein reported. These grains were identified and studied with the use of transmission electron microscopy (TEM), electron diffraction analysis...
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HAADF image of iron carbonitride, Fe9(N0.8C0.2)4, with lamellae of iron carbide, Fe7C3, hosted as an inclusion in diamond. In the lower left part of the image an idiomorphic crystal with spinel-type structure is observed intergrown with carbonitride. The volume below this grain is filled with redeposited Ga and sputtered material; originally it was likely filled with trapped fluid and/or vapor. The outlined square area corresponds to regions for Si and C elemental maps (Fig. 5). Circles show areas for which EDX spectral analyses were determined. Foil no. 4588. (Color online.)
Published: 01 August 2017
Figure 3. HAADF image of iron carbonitride, Fe 9 (N 0.8 C 0.2 ) 4 , with lamellae of iron carbide, Fe 7 C 3 , hosted as an inclusion in diamond. In the lower left part of the image an idiomorphic crystal with spinel-type structure is observed intergrown with carbonitride. The volume below
Image
Iron carbide lamellae in foil no. 4588. (a) HAADF image of two iron carbide lamellae within the iron carbonitride grain included within diamond. The areas over which EDX analyses were determined are shown in red squares (1 = a brighter contrasted volume within the lamella; 2 = the gray matrix of the lamella). The bright lines in the hosting carbonitride are dislocation lines. (b) EEL spectrum of the matrix of the thick lamella. The calculated ratio of Fe/C from this spectrum is 2.46, which is close to the ideal value of 2.33 for Fe7C3. (c and d) EDX spectra of iron carbide, Fe7C3 (c) from matrix without admixture of Si; (d) from bright area no. 1 with a noticeable admixture of Si. (Color online.)
Published: 01 August 2017
Figure 4. Iron carbide lamellae in foil no. 4588. ( a ) HAADF image of two iron carbide lamellae within the iron carbonitride grain included within diamond. The areas over which EDX analyses were determined are shown in red squares (1 = a brighter contrasted volume within the lamella; 2
Image
Drift-corrected elemental map of the Fe7C3 lamellae within carbonitride hosting a cubic grain of SiC. Foil no. 4588. (Color online.)
Published: 01 August 2017
Figure 5. Drift-corrected elemental map of the Fe 7 C 3 lamellae within carbonitride hosting a cubic grain of SiC. Foil no. 4588. (Color online.)
Journal Article
Published: 01 December 2019
American Mineralogist (2019) 104 (12): 1781–1787.
... be the most nitrogen-rich iron compound under core conditions. An iron carbonitride Fe 7 (C,N) 3 found as a mantle-derived diamond inclusion implies that β-Fe 7 N 3 and Fe 7 C 3 may form a continuous solid solution in the mantle deeper than 1000 km depth. Diamond formation may be related to the presence...
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Journal Article
Published: 01 September 2017
American Mineralogist (2017) 102 (9): 1769–1770.
...Dmitry A. Zedgenizov; Konstantin D. Litasov In the highlighted paper, Kaminsky and Wirth (2017) present new data on unique inclusions of iron nitrides and carbonitride in association with iron carbide, silicon carbide, and exotic Cr-Mn-Fe oxides in a “superdeep” diamond from Rio Soriso...
Image
Indexed electron-diffraction patterns (FFT) from HREM images of iron carbide grains. A) Fe2C crystal in foil #2025 with the zone axis [001]. B) Fe3C crystal in foil #2053 with the zone axis [101]. C) Fe2C crystal in foil #2053 with the zone axis [001]. Note the presence of weak additional spots between (h00) reflections and (010) and (210) reflections, which can be indexed as (100) and (110) reflections. D) Iron carbonitride in foil # 2053 with the zone axis [010].
Published: 01 April 2011
additional spots between ( h 00) reflections and (010) and (210) reflections, which can be indexed as (100) and (110) reflections. D) Iron carbonitride in foil # 2053 with the zone axis [010].
Image
Indexed electron-diffraction patterns (FFT) from HREM images of iron carbide grains. A) Fe2C crystal in foil #2025 with the zone axis [001]. B) Fe3C crystal in foil #2053 with the zone axis [101]. C) Fe2C crystal in foil #2053 with the zone axis [001]. Note the presence of weak additional spots between (h00) reflections and (010) and (210) reflections, which can be indexed as (100) and (110) reflections. D) Iron carbonitride in foil # 2053 with the zone axis [010].
Published: 01 April 2011
additional spots between ( h 00) reflections and (010) and (210) reflections, which can be indexed as (100) and (110) reflections. D) Iron carbonitride in foil # 2053 with the zone axis [010].
Image
Indexed electron-diffraction patterns (FFT) from HREM images of iron carbide grains. A) Fe2C crystal in foil #2025 with the zone axis [001]. B) Fe3C crystal in foil #2053 with the zone axis [101]. C) Fe2C crystal in foil #2053 with the zone axis [001]. Note the presence of weak additional spots between (h00) reflections and (010) and (210) reflections, which can be indexed as (100) and (110) reflections. D) Iron carbonitride in foil # 2053 with the zone axis [010].
Published: 01 April 2011
additional spots between ( h 00) reflections and (010) and (210) reflections, which can be indexed as (100) and (110) reflections. D) Iron carbonitride in foil # 2053 with the zone axis [010].
Image
Indexed electron-diffraction patterns (FFT) from HREM images of iron carbide grains. A) Fe2C crystal in foil #2025 with the zone axis [001]. B) Fe3C crystal in foil #2053 with the zone axis [101]. C) Fe2C crystal in foil #2053 with the zone axis [001]. Note the presence of weak additional spots between (h00) reflections and (010) and (210) reflections, which can be indexed as (100) and (110) reflections. D) Iron carbonitride in foil # 2053 with the zone axis [010].
Published: 01 April 2011
additional spots between ( h 00) reflections and (010) and (210) reflections, which can be indexed as (100) and (110) reflections. D) Iron carbonitride in foil # 2053 with the zone axis [010].
Journal Article
Published: 01 April 2025
American Mineralogist (2025) 110 (4): 506–512.
... in ε-Fe 3 N does not alter its structure, resulting in the formation of iron carbonitride ε-Fe 3 (C,N) ( Jack 1948 ). In Fe 3 C, iron atoms adopt an hcp arrangement, while carbon atoms occupy a trigonal prismatic site. This configuration leads to a very low solubility of nitrogen in Fe 3 C under...
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Journal Article
Published: 01 April 2011
The Canadian Mineralogist (2011) 49 (2): 555–572.
... additional spots between ( h 00) reflections and (010) and (210) reflections, which can be indexed as (100) and (110) reflections. D) Iron carbonitride in foil # 2053 with the zone axis [010]. ...
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Journal Article
Published: 22 June 2015
The Canadian Mineralogist (2015) 53 (1): 83–104.
... at.%, with the N/(C+N) ratio varying from 0.37 to 0.60. These minerals, in fact, are not carbides, but nitrocarbides and carbonitrides. Nitrogen also occurs as fluid inclusions ( Kaminsky et al . 2013 , and this study - see Fig. 1d ). These facts suggest the importance of nitrogen in the lower mantle...
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Journal Article
Published: 03 April 2023
American Mineralogist (2023) 108 (4): 653–658.
... greater than 250 km ( Rohrbach et al. 2007 ). Based on the presence of iron nitrides and carbonitrides in meteorites and deep diamond inclusions, nitrogen may be distributed heterogeneously and enriched in metal phases in the Earth’s interior ( Li and Keppler 2014 ; Litasov et al. 2017 ; Rubin and Ma...
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Journal Article
Published: 01 March 2014
European Journal of Mineralogy (2014) 26 (1): 53–59.
.... Marshintsev V.K. ( 1995 ): Carbon isotopic composition and origin of SiC from kimberlites of Yakutia, Russia . Geochim. Cosmochim. Acta , 59 , 781 – 791 . Mazzoni A.D. Aglietti E.F. ( 1997a ): Carbonitriding of andalusite: phases involved and reaction mechanism . Materials Chem. Phys...
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Journal Article
Journal: Geology
Published: 12 December 2017
Geology (2018) 46 (2): 171–174.
... the NASA Stardust mission to comet 81P/Wild 2 ( Chi et al., 2009 ). At site 2, the V-Nb-osbornite is probably a carbonitride, because it contains 11 wt% carbon. Pure osbornite (TiN) is an extremely rare mineral that has been found extraterrestrially as comet dust ( Chi et al., 2009 ) or as trace...
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Journal Article
Published: 16 April 2025
American Mineralogist (2025)
...). However, N quantification has to be considered as just 242 qualitative and with no other evidence, this hypothesis can be supported. Earlier, we demonstrated the 243 significant role of nitrogen in deep Earth, where it forms nitrides, carbonitrides (Kaminsky and Wirth, 244 2017) and even native nitrogen...
Journal Article
Published: 01 April 2021
Clays and Clay Minerals (2021) 69 (2): 254–262.
... photocatalysis in nitrogen-doped titanium oxides . Science , 293 , 269 – 271 . Chagas , C. A. , Pfeifer , R. , Rocha , A. B. , & Teixeira da Silva , V. ( 2012 ). Synthesis of niobium carbonitride by thermal decomposition of guanidine oxaloniobate and its application...
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Journal Article
Journal: Elements
Published: 01 December 2014
Elements (2014) 10 (6): 441–446.
...) carbides, titanium carbonitrides, SiC, nickel and iron silicides, refractory metal nuggets (RMNs), iron-rich metal (FeNiSi), and intergrowths of these ( Bernatowicz et al. 2006 ). In many cases, the other phases form as coatings or subgrains on existing TiC surfaces. Sometimes multiple iron-rich metal...
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Journal Article
Published: 01 September 2013
European Journal of Mineralogy (2013) 25 (3): 373–383.
... , 599 – 600 . Khabashesku V.N. Margrave J.L. ( 2002 ): Carbonitride nanomaterials, thin films and solids . Adv. Eng. Mater. , 4 ( 9 ), 671 – 675 . Khvostantsev L.G. Vereshchagin L.F. Novikov A.P. ( 1977 ): Device of toroid type for high pressure generation . High...
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