Abstract
External and internal morphologies of natural impact apographitic diamonds (paramorphoses) have been studied. The (0001) surface morphology of the paramorphoses reflects their phase composition and the structural relationship of its constituting phases. Growth and etch figures together with the elements of crystal symmetry of lonsdaleite and diamond are developed on these surfaces. The crystal size of lonsdaleite is up to 100 nm, and that of diamond is up to 300 nm. Two types of structural relations between graphite, lonsdaleite, and diamond in the paramorphoses are observed: the first type (black, black-gray, colorless and yellowish paramorphoses): the (0001) graphite face is parallel to the (100) lonsdaleite face and parallel to (111) diamond; the second type (milky-white paramorphoses): the (0001) graphite is parallel to the (100) lonsdaleite and parallel to the (112) diamond. The first type of the paramorphoses contains lonsdaleite, diamond, graphite or diamond, lonsdaleite, the second type of the paramorphoses contains predominantly diamond. The direct phase transition of graphite → lonsdaleite and/or graphite →diamond occurred in the paramorphoses of the first type. A successive phase transition graphite → lonsdaleite → diamond was observed in the paramorphoses of the second type. The structure of the paramorphoses of this type shows characteristic features of recrystallization.
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Valter, A.A., Erjomenko, G.K., Kvasnitsa, V.N., and Polkanov, Yu.A., Udarno-metamorfogennye mineraly ygleroda(Shock-metamorphogenetic carbon minerals), Kiev: Naukova Dumka, 1992.
Vishnevsky, S.A., Afanasyev, V.P., Argunov, K.P., and Palchik, N.A., Impactnye almazy: ikh osobennosti, proiskhozhdenie i znachenie (Impact diamonds: their features, origin and significance), Novosibirsk: izd. SIC Siberian Branch of RAS, 1997.
Langenhorst, F., Shafranovsky, G.I., Masaitis, V.L., and Koivisto, M., Discovery of impact diamonds in a Fennoscandian crater and evidence for their genesis by solid-state transformation, Geology, 1999, vol. 27, no. 8, pp. 747–750.
Koeberl, C., Masaitis, V.L., Shafranovsky, G.I., et al., Diamonds from the Popigai impact structure, Geology, 1997, vol. 25, no. 11, pp. 967–970.
Gorogotskaya, L.I., Kvasnitsa, V.N., and Nadezhdina, Ye.D., Orientational relations of graphite–lonsdaleite–diamond at natural transformations in shock waves, Mineral. J. (Ukraine), 1989, vol. 11, no. 1, pp 26–33.
Kurdyumov, A.V. and Pilyankevich, A.N., Fazovye prevrashcheniya v uglerode i nitride bora (Phase transformations in carbon and boron nitride), Kiev: Naukova Dumka, 1979.
Godinho, J.R., Piazolo, S., and Evans, L.Z., Effect of surface orientation on dissolution rates and topography of CaF2, Geochim. Cosmochim. Ac., 2012, vol.86, pp. 392–403.
Godinho, J., Piazolo, S., and Balic-Zunic, T., Importance of surface structure on dissolution of fluorite: implications for surface dynamics and dissolution rates, Ibid., 2014, vol. 126, pp. 398–410.
Kvasnytsya, V. and Wirth, R., Micromorphology and internal structure of apographitic impact diamonds: SEM and TEM study, Diam. Relat. Mater., 2013, vol. 32, pp. 7–16.
Wirth, R., Focused ion beam (FIB): A novel technology for advanced application of microand nanoanalysis in geoscience and applied mineralogy, Eur. J. Mineral., 2004, vol. 16, pp. 863–876.
Wirth, R., Focused ion beam (FIB) combined with SEM and TEM: advanced analytical tools for studies of chemical composition, microstructure and crystal structure in geomaterials on a nanometer scale, Chemical Geology, 2009, vol. 261, pp. 217–229.
Trimby, P.W., Orientation mapping of nanostructured materials using transmission Kikuchi diffraction in the scanning electron microscope, Ultramicroscopy, 2012, vol. 120, pp. 16–24.
Wyckoff, R.W.G., Crystal Structures, 2nd ed., vol. 1, pp. 7–83, New York: John Wiley and Sons, 1963.
Valter, A.A., Oleinik, G.S., Fisenko, A.V., and Semenova, L.F, Structural and morphological evidence of the impact-induced development of diamond after graphite in the Novo-Urei meteorite, Geochemistry Int., 2003, vol. 41, pp. 939–946.
Nakamuta, Y. and Toh, S., Transformation of graphite to lonsdaleite and diamond in the Goalpara ureilite directly observed by TEM, Am. Mineral., 2013, vol. 98, pp. 574–581.
Garvie, L.A.J., Németh, P., and Buseck, P.R., Transformation of graphite to diamond via a topotactic mechanism, Ibid., 2014, vol. 99, pp. 531–538.
Wheeler, E.J. and Lewis, D., The structure of a shock-quenched diamond, Mater. Research Bulletin, 1975, vol. 10, no. 7, pp. 687–694.
Bundy, F.P. and Kasper, J.S., Hexagonal diamonda new form of carbon, J. Chem. Phys., 1967, vol. 46, no. 9, pp. 3437–3446.
Lonsdale, K., Formation of lonsdaleite from single-crystal graphite, Am. Mineral., 1971, vol. 56, pp. 333–336.
Sokhor, M.I. and Futergendler, S.I., X-ray crystallographic study of diamond-lonsdaleite crystals, Crystallography, 1974, vol. 19, no. 4, pp. 759–762.
Kurdyumov, A.V., Malogolovets, V.G., Novikov, N.V., et al., Polimorfnye modifikatsii ugleroda i nitrida bora (Polymorphic modifications of carbon and boron nitride), Moscow: Metallurgiya, 1994.
Oleinik, G.S., Valter, A.A., and Erjomenko, G.K., The structure of high lonsdaleite diamond grains from the impactites of the Belilovka (Zapadnaja) astrobleme (Ukraine), 34th Lunar and Planetary Sci. Conf. LPI, 17–21 March, 2003, Houston, Texas, USA, Abstr. no.1561.
Kurdyumov, A.V., Britun, V.F., Yarosh, V.V., et al., The influence of the shock compression conditions on the graphite transformations into lonsdaleite and diamond, J. Superhard Mater., 2012, vol. 34, no. 1, pp. 19–27.
Masaitis, V.L., Impaktnye almazy Popigaiskoi astroblemy: ikh osnovnye svoistva i promyshlennoe primenenie (Impact diamonds of Popigai astrobleme: their principal features and industrial uses), Proc. Rus. Mineral. Soc., 2013, vol. 142, no. 2, pp. 1–10.
Trueb, L.F., An electron-microscope study of shock-synthesized diamond, J. Appl. Phys., 1968, vol. 39, no. 10, pp. 4707–4716.
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Kvasnytsya, V., Wirth, R., Piazolo, S. et al. Surface morphology and structural types of natural impact apographitic diamonds. J. Superhard Mater. 38, 71–84 (2016). https://doi.org/10.3103/S1063457616020015
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DOI: https://doi.org/10.3103/S1063457616020015